Source: Statistics Denmark Today, more than 10% of the demand for energy is supplied by renewable energy. The renewable energy resources are mainly wind energy and biomass, which are used to produce electricity, combined heat and power, or district heating. Internationally, Denmark is among the leading nations in wind energy. Table 2.4:
Source: Danish Energy Authority Energy consumption Despite the economic growth, total energy consumption has remained largely unchanged at approximately 800 PJ in the last ten-year period, cf. tables 2.6 and 2.7. Denmarks dependence on oil and coal has fallen. Particularly in the production of electricity and heat, oil and coal have been substituted with other fuels. Thus, natural gas, waste and biomass are increasingly being used in small-scale and industrial CHP plants, natural gas and renewable energy is increasingly being used in large scale electricity production, and natural gas is increasingly being used for individual heating of buildings. Figure 2.5 shows adjusted energy consumption, sector by sector. In the last 20 years relative consumption by the transport sector has risen, whereas relative domestic sector consumption has fallen. Structure of the market The structure of the market in the energy sector is characterised by a division between electricity, gas, and district heating supply. Table 2.5:
Source: Danish Energy Authority Table 2.6:
Source: Danish Energy Authority Table 2.7:
Source: Danish Energy Authority More than two-thirds of Denmarks electricity supply comes from large primary power stations and CHP plants. Just under one-third is supplied by small-scale and industrial CHP plants and wind turbines. The large primary power stations are organised in two companies, which are owned by around 80 regional grid companies whose owners are municipalities, limited liability cooperatives, independent institutions, etc. The small-scale plants are primarily organised in municipally owned and consumer-owned district heating companies. The wind turbines are primarily privately owned or owned by the electricity companies.
Figure 2.5: Source: Danish Energy Authority In connection with the implementation of the EU Directive on liberalisation of the electricity sector, a reform of the sector has been carried out. As part of the reform, the market was fully opened on 1 January 2003, which means that all electricity customers can now use the electricity supplier of their choice.
Figure 2.6: Source: Danish Energy Authority Most production of natural gas and oil is taken care of by a private company, DUC (Dansk Undergrunds Consortium), while the state-owned company DONG (Dansk Olie og Naturgas) takes care of the transportation of natural gas to the shore. DONG also owns and operates the national transmission grid for natural gas and part of the distribution grid. In addition, three regional gas companies under municipal ownership, own and operate regional natural gas grids, with distribution to the end users. In the gas sector, too, a law reform has been passed to implement the EU Directive on liberalisation of the gas market, and the governments aim is for the gas market to be open for all gas customers from 1 January 2004. Approximately half of the demandfor heating is supplied by district heating. The heat is supplied from primary and small-scale CHP plants, waste incineration plants and biomass-fired district heating stations. Apart from the primary plants, the plants are owned either by municipalities or by local cooperatives that are owned by the consumers. Initially, district heating will not be covered by the liberalisation process, but the government will investigate whether it is possible in the longer term to have a more free choice of supplier in areas with large, interconnected district heating grids. Prices and taxes Energy prices are one of the key factors governing energy consumption. In 2000 total spending on energy, including taxes and VAT, amounted to DKK 118.1 billion. Of this figure, domestic users paid DKK 56.2 billion, manufacturing industries DKK 27.7 billion, and the commercial sector and the service industries, including public services, DKK 24.5 billion. As a general rule, enterprises subsequently receive a full refund of energy taxes and VAT, but not of CO2 taxes. Figures 2.6 and 2.7 show the energy prices paid by domestic users. Figure 2.6 shows the current consumer prices, including taxes and VAT. Figure 2.7 shows the development in fixed 2001 prices. The fixed prices have been adjusted for the change in general prices according to the consumer price index. The prices of heating oil and natural gas follow each other because this is laid down by law. The tax on petrol has varied considerably over time, which has affected the price of petrol. Measured in fixed prices, the prices of petrol, heating oil and natural gas fell from 1980 until the early 1990s, cf. figure 2.7. The price of electricity remained relatively constant for the whole of the period, although with a rising trend in the later years, primarily because of higher taxes. As an added incentive to enterprises to improve their energy efficiency, a green tax package with gradually increasing CO2 and energy taxes was introduced in 1996. Enterprises with a particularly high energy consumption can contract with the Danish Energy Authority on energy-efficiency improvements in return for a discount in the CO2 taxes. In 2000 the revenue from energy taxes amounted to DKK 33.0 billion, up from DKK 31.9 billion in 1999. The largest contribution, DKK 10 billion, comes from petrol. Total revenue has increased by 140% in relation to 1990, when there were no CO2 and sulphur taxes. In 2000 energy taxes accounted for more than 5% of total tax revenue.
Figure 2.7: Source: Danish Energy Authority
Figure 2.8: Source: Danish Energy Authority Trade In 2000 net foreign exchange earnings from energy products amounted to DKK 13.1 billion. There was a profit on the trade in oil, natural gas, and electricity, but a loss on the trade in coal. 2.1.7 TransportEfficient and flexible transportation of goods and persons is a vital element of the foundation of the modern welfare society. At the same time, transport is in itself an important economic sector that contributes to economic growth, employment, and foreign exchange earnings. The positive effects of the transport sector must be seen against the fact that the sector burdens society in different areas traffic accidents, air pollution, noise, congestion, and CO2 emissions. In Denmark, this burden has been reduced in some important areas primarily in the form of better traffic safety and less air pollution at the same time as traffic has increased. Table 2.8: However, there has not been a corresponding development with respect to CO2, and the transport sector has not yet succeeded in decoupling economic growth and greenhouse gas emissions, as has been done in the energy sector. Transport activity, energy consumption and CO2 emissions within the transport sector have developed largely in step with economic growth. One reason for this is that a number of measures that have been used in other sectors, e.g. the energy sector, including efficiency improvement and substitution of energy sources, have not been directly available or have been associated with heavy costs in the transport sector. The developments in passager and goods transport activities are shown in table 2.9 and 2.10 respectively In 2001 the transport sectors CO2 emissions were approximately 18% higher than the level in 1990. In 2001 the transport sector accounted for about 22% of Denmarks total CO2 emissions. Its contribution to Denmarks total greenhouse gas emissions are calculated as a share of the total emissions of greenhouse gases, which include industrial gases, methane, and nitrous oxide. Calculated in this way, the sector is responsible for about 18% of total emissions. The trend in CO2 emissions in the transport sector is therefore of considerable importance to the total trend in the greenhouse gas emissions. Table 2.9:
Source: Ministry of Transport Table 2.10:
Note: 1 Pipelines not included 2.1.8 Business sectorIn Denmark the production value of industry is approximately 30% of total national production. Table 2.11 shows that the largest industries in Denmark are the food, drink and tobacco, engineering, electronics, and the chemical industry. The business sector as a whole (industry, building and construction, and public and private services) accounts for around 13% of Denmarks total emissions of greenhouse gases. CO2 from energy consumption accounts for by far the largest part of these emissions, but the sector is also a direct source of emissions of industrial greenhouse gases. In Denmark, the industrial sectors energy consumption accounts for about 20% of total energy consumption. This 20% does not include energy consumption for transport and space heating. The sectors energy consumption has varied greatly over the last 20 years. Up to 1983, consumption fell considerably due to increases in the price of oil. When oil prices fell in 1986, energy consumption began rising again. In the period 1990-2001 energy consumption in the industrial sector rose by just under 9%, while electricity consumption in the same period increased by almost 22%.From 2000 to 2001 energy consumption rose by just under 2% owing to a considerably higher level of activity. Since 1994 energy consumption per produced unit has fallen,see figure 2.9. Table 2.11:
Source: Statistics Denmark The main action against the industrial sectors energy consumption has hitherto been based on the green tax package for businesses passed by the Folketing in 1995. The package contained a combination of taxes and rebates to enterprises through, among other measures, government grants to promote energy savings by enterprises.
Figure 2.9: Source: Danish Energy Authority and Odyssee The development in the last few years since the introduction of the green tax package shows that it is possible to increase industrial growth without a corresponding increase in energy consumption and CO2 emissions. On the contrary, during increased growth it has proven possible to keep energy consumption constant and reduce CO2 emissions from energy consumption by the industrial sector. For industrial greenhouse gases (HFCs, PFCs and SF6), regulation through taxes, and rules on phasing out the use of these substances have been implemented. With certain exceptions, the phasing-out process is expected to take place in the period 2003-2006. 2.1.9 WasteThe waste sectors contribution to the emissions of greenhouse gases consists only of methane. Methane emissions come from the decomposition of organic waste at landfill sites. Emissions of the industrial gases HFC and SF6 from disposal of, for example, refrigerators and certain thermal glazing, which contain these substances, are included under the business sector. There are also CO2 emissions in connection with disposal of oil-based products, e.g. packaging, plastic bags, etc. Since waste incineration in Denmark is included in energy production, these CO2 emissions must be included under the energy sector in accordance with the inventory rules from the IPCC. Methane emissions from the waste sector are expected to fall in the future because the municipalities are now obliged to assign all waste suitable for incineration to incineration plants. This means that only a small quantity of organic waste will be deposited at landfills compared with the quantity deposited before the introduction of this obligation in 1997. In addition, gas from a number of landfills is being used in energy production, which contributes to reducing both CO2 and methane emissions. Table 2.12:
Source: Statistics Denmark Finally, in connection with incineration, some of the waste is used as an energy source. As many of the incineration plants as possible have been converted to CHP production. In other words, the heat is used to supply district heating, and the electricity is sold to electricity suppliers. In 2001, 32 incineration plants in Denmark converted 25% of the entire waste production and contributed 3% of the entire Danish energy production. 2.1.10 Buildings and urban structureOne-twentieth of the area of Denmark is urbanised. 85% of Danes are town-dwellers, and most enterprises, institutions, etc., are situated in owns. Many pollution problems are therefore concentrated in the towns. Today, the total built-up area is 654 mill. m2. Table 2.12 shows the distribution of the area between housing, factories, offices, etc. Today, about 16,000 homes are built per year, which is one-third of the number built in the first half of the 1970s. House building is expected to remain at this level. In recent years, house building has accounted for slightly more than half of all investment in building activities, and about half of the investment in the housing sector has gone on alterations and extensions. Building for industry and commerce now accounts for around half of all building in towns. Table 2.13:
Source: Statistics Denmark Towns and cities are generally characterised by separation of residential and industrial areas, industrial buildings being situated in specially designated zones on the outskirts of the towns. The growth in the service industries and the growth in manufacturing with a small environmental impact imply new possibilities for integrating industry and housing, thereby reducing the need for transport between home and work. Table 2.14:
Source: Danish Institute of Agricultural Sciences, Danish Research
Institute of Food Economics, Statistics Denmark. Approximately two-thirds of the total building space is heated. The main forms of heating are district heating and central heating based on oil and natural gas. Half of the heated space is heated by district heating and, as seen from table 2.13, the use of both district heating and natural gas has increased at the expense of oil. 2.1.11 AgricultureIn the last 40 years the area used for agriculture has fallen from 72% (30,900 km2) of the total area in 1960 to 62% (26,756 km2) in 2000. Table 2.14 shows the breakdown by type of crop over the last 30 years. The proportion of agricultural land under grass and greenfeed in rotation and permanent grass fell considerably from 1970 to 1990, but rose considerably during the 1990s, due partly to increasing use of grass fields for dairy farming, and partly to the change in EU subsidy schemes, which means that grass or industrial seed must be grown on set-aside land. From 1980 to 2001 the number of farms fell from 119,155 to 53,489. In the same period the average size of farms increased from 24 ha to 50 ha. This development has reduced the importance of agriculture to employment and the national economy. However, agricultural production has grown, both in quantity and value, and agricultural exports still make up a large proportion - 11% - of Denmarks total exports. During the 1990s interest in organic farming increased considerably. In 2001 organic farms accounted for approximately 5% of land under cultivation. In the last 30 years use of nitrogen by agriculture has varied greatly, cf. table 2.14. Up to 1990 there was a big increase in the use of nitrogenous fertiliser, but during the 1990s use of this type of fertiliser fell considerably, and in 2001 nitrogen consumption was below the 1970 level. The nitrogen content of manure has probably remained approximately unchanged in the entire period in question. Consumption of phosphorus and potassium in fertilisers fell throughout the period. The cattle population fell by 33% from 1970 to 2001, cf. table 2.14. Most of the cattle are dairy cows. Since milk production remained approximately unchanged throughout the period, the fall in cattle population is due to higher productivity per animal. In the same period, the pig population increased by 51%. The sheep population has doubled in relation to 1970, while after falling during the 1980s, the poultry population is now higher than it was in 1970. Agriculture was responsible for 20% of Denmarks total emissions of greenhouse gases in 2001. The proportion is expected to be down at 16% in 2010. The gases are mainly methane and nitrous oxides. CO2 from fuel consumption in the agricultural sector accounts for 3.6% of total Danish emissions. 2.1.12 ForestryApproximately 11% of Denmark is forested. Originally focus was mainly on the potential of conifers, but in recent years focus has changed towards indigenous, deciduous tree species as offering greater long-term production and nature potential. Denmarks forests are managed as closed canopy forests. The main objective is to ensure sustainable and multiple-use management of the forests and to manage them in line with the overall management of the countryside. Instead of clear-cut systems, forest owners are to a higher degree applying near-to-nature forest management regimes. Unlike our Scandinavian neighbours, Denmark is not a country in which forestry plays an important role in the national economy. The Danish Forest Act protects a very large part of the existing forests against conversion to other landuses. Afforestation, for which public subsidies are made available, is as standard protected as forest reserve. In principle, this means that most of the forested land in Denmark will remain as forest. A target has been set of 20-25% of Denmark being forest landscapes by the end of the 21st century. A considerable increase in the forest area is therefore to be achieved. Denmark is the only part of the Kingdom in which forestry is practised. Greenland and the Faroe Islands have almost no forest. 2.2 Greenland2.2.1 Form of government and administrative structureGreenland has had home rule since 1979. The Home Rule Government consists of a directly elected parliament (the Landsting), comprising 31 members. A general election is held every four years. The Landsting elects a government (the Landsstyre), which is responsible for the central administration under the Prime Minister (the Landsstyreformand). The members of the government head the various ministries. However, since Greenland is part of the Kingdom of Denmark, some fields of responsibility remain under the state, including the Constitution, the right to vote, eligibility for election to the Folketing, the administration of justice, the concept of citizenship, foreign policy and the National Bank. The Home Rule Government is responsible for other areas, including transport and communication, and the environment and nature. Greenland is not a member of the EU, but has an OCT scheme (Overseas Countries and Territories scheme) that ensures the country open access to the European market for its fish products. International agreements entered into by the Danish government also cover Greenland and apply to Greenland to the same extent unless the Home Rule Government specifically requests exemption or deviation from them. Denmarks ratification of the Climate Convention and the Kyoto Protocol both cover Greenland. 2.2.2 PopulationGreenland has a population of slightly more than 56,000, 88% of which were born in Greenland. Most of the remainder of the population comes from Denmark. Fishing is the main industry, and it is estimated that about 2,500 people are directly employed by it. In addition, around 3,000 people work in the fisheries industry and derivative occupations. 2.2.3 GeographyWith an area of 2.2 mill. km2, Greenland is the worlds largest island. It extends over almost 24 latitudes. Nordpynten lies only 700 km from the North Pole, and Kap Farvel, 2,600 km further south, is level with Oslo. Towards the south, the height of the sun and thus the length of day and night are almost as in Denmark. Towards the north there is the midnight sun and winter darkness, both lasting for two thirds of the year. 85% of Greenland is covered by a continuous, slightly convex ice cap, which reaches a height of more than 3,000 m above sea level. In a borehole drilled in the central part of the ice cap, the drill reached a depth of 3,030 m in the bedrock. The remaining 15% of the island is home to Greenlands flora and fauna, and here, on the edge of the ice cap, the people live mainly in the coastal areas, from which there is access to open water. 2.2.4 ClimateGreenlands northern location and the cold and more or less ice-filled seas that surround it are the main reasons for its cold climate. Greenland has a mostly arctic climate, and forests cannot grow there. Particularly the northern part of the country is close to the North American continent, separated from it by only a relatively narrow and ice-filled sea. The position of south Greenland, on the other hand, means that the climate here is influenced by the North American continent to the west, and the ocean to the east. Atmospheric pressure Atmospheric pressure is generally highest in April/May. The weather in Greenland is most stable at this time of year. After this, in the summer months, the variation in atmospheric pressure is small, but in winter it is much greater, with a generally higher atmospheric pressure towards the north than towards the south, leading to a higher frequency of cold winds from northerly directions and higher wind velocities. The biggest pressure extremes in Greenland occur in the winter period because of the great temperature contrasts in the atmosphere. The highest atmospheric pressure measured in Greenland was 1059.6 hPa, which was recorded in January 1958. The lowest was 936.2 hPa, recorded in 1986 and 1988. Wind Storms typically occur in connection with the passage of low-pressure systems. Between these systems, there are undisturbed periods of varying duration throughout the year, when the wind is governed by local conditions. An example is the ice caps katabatic wind system, the extent of which is enormous. A katabatic wind is a wind that blows down an incline, moving from the central part out towards the edge. The wind velocity accelerates with increasing incline of the surface, and the topography can cause channelling, resulting in an extremely high velocity at the edge of the ice. Greenland has many days with little or no wind. In some places on the east coast this is the case for 60% of the time. Gusts can be very strong. Gusts of up to 75.1 m/s were measured in Danmarkshavn in 1975, but even stronger gusts undoubtedly occur in connection with the so-called piteraqs. These fall winds, which are katabatic, locally channelled winds from the ice cap, occur in several locations in Greenland, and are characterised by a very abrupt change from light wind to storm. In Greenlandic, piteraq means "that which assaults one". Figure 2.10 : Figure 2.11 : Temperature The summer temperatures on both the west and the east coast differ by only a few degrees from south to north, despite a distance of more than 2,600 km. The reason for this is the summer midnight sun in north Greenland. Conversely, winter darkness and the absence of warm sea currents mean that the temperature during the winter period differs considerably from north to south. There is also a big difference in the temperature conditions at the outer coast and inside the fjords. In summer, drift ice and the cold water along the coast can mean that it is warmer inside the fjords, while in winter, on the other hand, the presence of the sea makes it warmer in the coastal areas than inside the fjords. Foehn winds can disturb this picture in the wintertime. Foehn winds are very common in Greenland, and in winter the hot, dry winds can cause the temperature to rise by 30ºC within a relatively short space of time, resulting in melting of snow and ice. The temperature record of 13.9ºC from 23 November 1987 in Nuuk is an example of the effect of a Foehn wind. The highest temperature recorded in Greenland since 1958 is 25.5ºC. It was recorded at the "ice cap" station in Kangerlussuaq in July 1990. In Greenland, frost can occur in all the months of the year except deep inside the fjords at Narsarsuaq Airport and Kangerlussuaq for a couple of the summer months. The "frostfree" period in southern Greenland varies from 60 to 115 days per year. The coldest place in Greenland is naturally on the ice cap, where the temperature can fall to below -70ºC. Temperatures in Greenland have shown a slightly rising trend for the last 125 years, although, on a shorter time scale, temperatures have generally fallen since the 1940s. This has been most marked on the west coast, where a rising trend has only been seen over the last few years. On the east coast, however, there has been a rising trend since the 1970s. Precipitation Recorded precipitation in Greenland decreases with rising latitude and from the coast to the inland area. Particularly for southern stations there is considerable seasonal variation. Right down in the south and particularly in the south-eastern region, precipitation is significant, average annual precipitation ranging from 800 to 2,500 mm along the coasts. Further inland, towards the ice cap, considerably less precipitation is recorded. In the northern regions of Greenland there is very little precipitation, from around 250 mm down to 125 mm per year. In a few places there are "arctic deserts", i.e. areas that are almost free of snow in winter, and where evaporation in summertime can exceed precipitation. Not surprisingly, snow is very common in Greenland. In fact, at most stations in the coastal region it can snow all year round without snow cover necessarily forming. There are thus many days with snow during the year, mostly in the southern part of the country. The snow depth is greatest in southern Greenland, averaging from one to more than two metres in all the winter months and sometimes reaching up to six metres. In southern Greenland the snow cover can disappear altogether during the winter in connection with warm Foehn winds. Towards the north, snow cover has already formed in most places by September and normally disappears again in June/July. Hours of sunshine The part of Greenland north of the Polar Circle, 66,5ºN, has midnight sun and polar night of varying length depending on the latitude. Midnight sun means that the sun is in the sky 24 hours a day, while polar night means that the sun does not rise above the horizon at all. Despite the polar night, the northern stations have more hours of sunshine than the southern stations. This is due to the "long" day, of course, but also to generally less cloud cover. However, although the surface of the soil receives more solar heat than in the tropics at around the summer solstice because of the long day, a considerable part of the energy is reflected because of the oblique angle of incidence and the snow- and icecovered surfaces. 2.2.5 EconomyPrincipal income for the Home Rule Government comes from transfers from the Danish state the so-called block grant. In addition, the Landsstyre and the municipalities have revenue from personal and corporate taxes, indirect taxes, and licences. There is no VAT. In addition, Greenland receives payment from the EU for access by EU fishermen to Greenlands fishing waters. Greenland uses the Danish currency, and Danish currency laws apply in connection with the transfer of funds between Greenland and other countries. This means that, in several areas, Greenland is affected by factors, e.g. interest and exchange rates that are determined by external factors. Exports 87% of Greenlands exports of DKK 2,251 million in 2001 consisted of fish products, 60% of which were prawns. The export value of fish products is heavily dependent on the prices on the world market. Although there was a considerably greater production of prawns in 2001, falling prices on the world market considerably reduced the export value. Imports Apart from fishery and hunting products, only a few goods are made in Greenland. Imports therefore include primarily all goods used in households, businesses and institutions, and for investment. In 2001 imports amounted to DKK 2,466 million. 2.2.6 EnergyAs in other modern societies, a large part of Greenlands CO2 emissions come from energy production and supply. Approximately 55% of all energy consumption is used for heating and electricity. Because of the big distances between towns in Greenland it is neither financially nor technically viable to establish a supply grid connecting them. This means that each town has its own power plant or CHP plant, and each village has its own power plant so-called island operation. At the same time, the climatic conditions mean that the towns cannot tolerate lengthy interruptions in their electricity supply. It is therefore also necessary to have reserve and emergency plants. Renewable energy Up to 1993 all energy production for electricity and district heating was based on diesel-driven power, heating and CHP plants. From 1993, when the hydropower station at Buksefjord went into operation, the capital Nuuk, where around 25% of the Greenlands population live, has been supplied with hydroelectricity for electric heating, lighting, and power. A small hydropower plant is now under construction in east Greenland, and a hydropower plant is planned in South Greenland. Together with heat utilisation from waste incineration plants, this means that in 2001 about 8% of Greenlands energy consumption (incl. transport, industry, etc.) came from renewable energy sources. Regular studies have been carried out with a view to utilising other renewable energy sources, but for various reasons, including the high requirements concerning security of supply, the forms of energy utilisation in question have not been of interest so far in Greenland. Heating Since 1993 all buildings built with public subsidies in Nuuk have been supplied with electric heating, and electric boilers with interruptible electric heating have been installed in existing district heating stations. The electric boilers operate as long as surplus electricity is available. When it is not, the oil boilers take over. The electricity for this is supplied at a competitive price. In the year 2001, 35% of all electricity produced in Greenland went to permanent and interruptible electric heat in Nuuk. In 10 towns the residual heat from electricity production is used for district heating. In addition, blocks of flats have their own individual heating plant, while most single-family houses have oil-fired central heating. In the villages, most of the houses have a central heating furnace or oil stoves. Electricity Nuuks electricity comes from the hydropower station. The electricity in the other towns and villages is produced at diesel-driven power plants. Work is going on to optimise the utilisation of the power plants. 2.2.7 TransportPassenger transport All passenger transport to and from Greenland is by air, via either Copenhagen-Kangerlussuaq or Copenhagen-Narsarsuaq. From Nuuk and Kangerlussuaq there is a connection via east Greenland to Iceland. Between towns and villages in Greenland, passenger transport is by passenger ship, aeroplane, or helicopter. Up through the 1990s both sea and air passenger traffic increased, and the increase in air traffic has resulted in a big rise in consumption of aviation fuel. There are bus services in the larger towns, while in the smaller ones, passenger transport is by taxi. To get out into the surroundings people usually use sailing boats and dinghies. There are around 5,000 dinghies in Greenland. The use of private cars, which is not deemed to have much effect on Greenlands CO2 emission, is increasing. In 1990, 1,410 ordinary cars were registered by private owners, while in 2001, the figure rose to 2,097 a 50% increase. Goods transport Almost all goods transport, both to and within Greenland, is by sea. A small proportion, mainly mail and perishable goods, is transported by air. 2.2.8 Business sectorThe principal industry in Greenland is fishing/fisheries. In 1996, 25% of the workforce was employed by this industry. In 2001 the fishing fleet and the land-based production facilities for fish, crabs and prawns accounted for about 30% of Greenlands entire energy consumption. The consumption is based mainly on fossil fuels. The industry is very sensitive to market fluctuations and it is therefore difficult to predict how it will develop. A large part of the rest of trade and industry consists of service enterprises. Except for electricity and district heating, energy consumption and CO2 emissions are not calculated separately for this part. Exploration for oil and minerals is under way. If large-scale extraction and production are started up at some time in the future, this could have a big effect on Greenlands CO2 emissions. There do not appear to be any enterprises using industrial gases in their production. 2.2.9 WasteApproximately 30,000 tonnes of waste are produced in Greenland each year. Three incineration plants in towns incinerate about 40% of the waste, while 47 small incineration plants in villages together incinerate 13%. Less than half of the waste is sent to landfills or burnt. Three new incineration plants are expected to go into operation in 2003, which will reduce the amount of waste sent to landfills/burnt to less than 25%. In the three existing incineration plants in towns, the heat from waste incineration is used for district heating. The heat from the three coming plants will be used in the same way, which means that the energy from more than 60% of Greenlands waste is expected to be utilised in 2003. The possibilities for reducing the quantity of waste sent to landfills/ burnt are being investigated. 2.2.10 Buildings and infrastructureThe government plays a very important role in the housing sector. Most housing is government housing or built with a government grant. Most private housing is built by the owners themselves, and the government offers grants for this purpose. The cooperative housing system was introduced in 1990 with government support. A large proportion of the houses are more than 15 years old, and a refurbishment programme has been initiated. This modernisation includes reducing the energy consumption of individual houses. 2.2.11 AgricultureGeographically, Greenlands agriculture is placed in the south and has a very limited impact on CO2 emissions. It consists mainly of sheep farming, and 25,000-30,000 lambs are produced each year. There are also two farms with domesticated reindeer. The number of sheep has remained relatively constant since 1990, whereas the number of domesticated reindeer has more than halved. The area farmed has increased by 85% since 1990 due to cultivation of a large quantity of coarse fodder. 2.2.12 ForestryThere is no forestry in Greenland apart from four experimental plantations with conifers, with a total area of 100 ha. 2.3 The Faroe Islands2.3.1 Form of government and administrative structureThe Faroe Islands have home rule status, and their internal affairs are governed by the Faroese parliament (the Lagting). The Faroe Islands are not a member of the EU. International agreements entered into by the Danish government cover the Faroe Islands and apply to them to the same extent unless the Faroese government specifically requests exemption or deviation from them. Denmarks ratification of the Climate Convention covers the Faroe Islands as well, but at the request of the Faroese government, geographical exemption was taken for the Faroe Islands in connection with Denmarks ratification of the Kyoto Protocol. 2.3.2 PopulationIn 2001 the Faroe Islands had a population of slightly less than 47,000 an increase of 5,000 since 1977. Net immigration was relatively small up to the beginning of the 1980s but increased relatively sharply in the years 1984-89 as a consequence of a high level of economic and employment activity. Table 2.15
Source: Grønlands Statistik and the Home Rules Department for Trade and Industry In the years 1990-1995 this picture changed to extensive emigration due to a serious deterioration in the economic and employment situation. In 1993 and 1994 alone, net emigration corresponded to 8% of the total population. Since 1996, the population has been growing. In 2001 the capital, Thorshavn, had a population of 18,000, corresponding to slightly less than 40% of the entire population. 2.3.3 GeographyThe Faroe Islands consist of 18 small, mountainous islands situated in the North Atlantic at about 62oN and 7oW. The islands extend over 113 km from north to south and 75 km from east to west, and the total area is 1,399 square kilometres. The highest points, almost 890 metres above sea level, are on the northern islands. 17 of the islands are inhabited. 2.3.4 ClimateThe climate on the Faroe Islands is strongly affected by the warm North Atlantic current and frequent passage of cyclones, which, depending on the location of the polar front, mainly come from southwest and west. The climate is characterised by mild winters and cool summers and is sometimes very damp and rainy. The high pressure over the Azores sometimes shifts towards the Faroe Islands. This can result in stable summer weather lasting several weeks, with quite high temperatures. In winter, on the other hand, the low pressure systems can move more southerly around the islands than normal, bringing in cold air from the north and a lengthy period of sunny winter weather. The maritime climate is also a result of the cold east Iceland current (polar current), which splits into two currents from eastern Iceland towards the Faroe Islands. The mixing of the water masses from this and the warm Gulf Stream causes a relatively big difference in the sea temperatures around the islands, and this in turn causes local variations in the climate. Atmospheric pressure The normal atmospheric pressure at sea level in Thorshavn is 1008 hPa on an annual basis, lowest from October to January (1004-1005 hPa) and highest in May (1014 hPa). The lowest atmospheric pressure recorded was 948.6 hPa on 11 January 1986, and the highest was 1046 hPa recorded on 20 February 1965. The islands have long periods with both low pressure and high pressure. The Faroe Islands lie close to the normal cyclone paths over the North Atlantic, and big and frequent changes in atmospheric pressure, with rises and falls of 20 hPa within 24 hours are common throughout the year. Sometimes, however, such violent cyclones develop that pressure falls of more than 24 hPA/24 hours occur. Temperature The annual mean temperature in Thorshavn is 6.5°C. The temperature in January and February is around 3.5°C, and in July and August, around 10.5°C. The annual mean temperature varies from place to place and is lowest at Vága Floghavn, 6.0°C, and highest in Sandur on the island of Sandoy, 7.0°C. In the 1990s the temperatures in Thorshavn exhibited a slightly rising trend. Precipitation Annual precipitation in Thorshavn is 1284 mm, most in autumn and least in summer. There are big geographical variations in precipitation, mainly due to the topography of the islands. It rains a lot on the Faroe Islands. Indeed, the Hvalvík has as much as 300 days with precipitation, and Thorshavn, 273 days. In the winter, precipitation is often in the form of snow. On average,Thorshavn has 44 days of snowfall per year, mostly in December and January. There is no snow at all in June, July, and August, but there can be snow in September. Precipitation in Thorshavn has exhibited a distinctly rising trend since the mid-1970s. Hours of sunshine, cloud cover and relative humidity Thorshavn has 840 hours of sunshine per year, most in May and June, the average being around 125 hours. In some Decembers there are no hours of sunshine at all. The highest number of hours of sunshine in a calendar month was 232 hours, observed in May 1948 and in May 2000. The location in the North Atlantic, combined with frequent low-pressure fronts, results in a large number of cloudy days (>80% cloud cover) 221 days in Thorshavn. The number of hours of sunshine in Thorshavn has remained stable for the last 20 years. The Faroe Islands have a moist climate, and the relative humidity is very high, 88% on an annual basis in Thorshavn. It is highest around August, and this is also when most fog occurs. Wind The mean wind is generally high on the Faroe Islands, particularly in autumn and winter (6-10 m/s). The wind is normally lightest in summer (4.5-6 m/s). There are normally no storms from April to August, while autumn and winter are windy, with many storms, some of which can reach hurricane force. The highest 10-minute mean winds are about 50 m/s, recorded at Mykines Lighthouse in March 1997 and January 1999. In 1997, gusts of almost 67 m/s were recorded at Mykines Lighthouse. Although the weather is generally windy, there are also still periods, mostly in summer and mostly of short duration. 2.3.5 EconomySince 1995 the Faroese economy has grown rapidly, due particularly to strong growth in fisheries. In 2001 exports increased by 12%, while imports fell by just under 4%, resulting in a surplus of DKK 160 million on the balance of trade. About 80% of exports from the Faroe Islands go to EU countries. Of this, Denmark accounts for 25% and the UK for 18%. In 2001 the Faroe Islands GNP was DKK 9.36 million. In the last few years, the Faroe Islands have turned a net foreign debt into a net credit balance, although with a big difference between the private and the public sector. At the end of 2001 the private sector had a net credit balance of more than DKK 5 billion, while the public sectors net foreign debt stood at almost DKK 3 billion. Unemployment has fallen sharply in the last few years and is now around 3%. Table 2.16 shows the development and breakdown by trade and industry, measured in gross national product at factor cost. In 2001 the surplus on the balance of payments, which, besides the balance of trade, includes services, wages, interest, transfers from the Danish state (approx. DKK 1.2 billion) and Danmarks Nationalbank, amounted to approximately DKK 900 million The Faroe Islands use the Danish currency and are part of the Danish currency area, although they have their own notes. 2.3.6 EnergyThe joint municipal company SEV is responsible for the production and sale of electricity on the Faroe Islands. In 2001, production amounted to about 230 mill. kWh. Of this, more than 30% was based on hydroelectricity, while the remainder was produced at diesel-driven plants. There is not much electricity production based on wind power only 0.3% or 0.5 mill. KWh in 2001. The reason for this is partly the very harsh wind conditions on the Faroe Islands, which make special demands on the wind turbines and thus the investment, and partly the fact that it is deemed difficult to adapt the great alternative production of this type to the relatively weak supply grid. Calculations show that there would be room for approximately 4.5 MW wind power in the grid in the area around Thorshavn. Table 2.16
Source: Færøernes Landsbank Table 2.17
Source: The Faroe Islands Ministry of Oil Of the electricity sold in 2001, 33% went to domestic users, 35% to industry, agriculture, and fisheries, 14% to the service sector, and the remainder to street lighting etc. Since a number of oil finds in British territorial waters close to the Faroese border in the 1990s, there has been a reasonable presumption that there is oil in Faroese territory, and the first licensing round was held in the spring of 2000. The first licences for exploration and production of hydrocarbons in the subsoil off the Faroe Islands were granted in August 2000. The first three exploration wells were drilled in the summer and autumn of 2001. In one of these, oil and gas were found. An evaluation programme is now being carried out to determine whether this find is commercially viable. 2.3.7 TransportGoods transport between the Faroe Islands and the rest of the world is mainly by sea. Two Faroese shipping companies operate freighter services all year round. Since 1998, the Smyril Line has carried freight in connection with their passenger winter sailings to Denmark. The Icelandic company EMISKIP also operates freight services throughout the year and has an office on the Faroe Islands. Besides Vagar Airport, the Faroe Islands have 12 helicopter pads. Air services are provided by MAERSK AIR, ICELAND AIR and the Faroese company ATLANTIC AIRWAYS. The number of air travellers to and from the Faroe Islands has risen sharply in the last few years. Passenger transport by sea takes place mainly in the summer period. There are both regular services (Smyril Line) and cruise liners. The number of foreign passenger ships calling at the Faroe Islands has been increasing in recent years. For 20-30 years up to the beginning of the 1990s and again over the last few years, major investments have been made in enlarging and modernising the transport infrastructure on the islands and the communication links with the outside world. Constructing roads, tunnels, and harbours is costly because of the difficult topographical conditions. Since an economic downturn at the beginning of the 1990s, the number of motor vehicles has increased by almost 1,000 and now stands at 21,000 motor vehicles, of which 16,000 are cars and 3,500 lorries and vans. 2.3.8 Business sectorExcluding exports of ships, which vary considerably over the years, 98% of the Faroe Islands export earnings comes from fish and fish products. The fishing industry is therefore of vital importance to earnings and employment on the Faroe Islands. The limited opportunities in other sectors of industry reinforce still further the totally dominant role of the fishing industry. Small villages in particular are almost entirely dependent on fisheries. In 2001 more than 27% of total wages on the Faroe Islands came from the fishing industry. Today, the number of man-years in the fishing fleet itself is estimated to be about 2,000. Besides the actual fish industry, a number of workshops and industrial enterprises have been built up to make equipment etc. for fishing vessels and the fisheries industry. This group includes shipyards and firms making fishing tackle, and machines and equipment for filleting factories. The last few years have seen the establishment of companies exporting fishing-system solutions to countries in the third world and elsewhere. The absence of a large domestic market, high transport costs for raw materials and finished goods, and in an international context - a relatively high level of overall costs have hitherto prevented the Faroe Islands from establishing export-oriented industries apart from the fishing industry and the firms supplying it. The Faroese government supports the development of small industry and manual trades based on sales to the domestic market. 2.3.9 Buildings and urban structureFor many years, the Faroese authorities have made every effort to counteract migration from the small or isolated villages and islands, in particular through a major road-building programme and other transport measures. However, population development is generally poorer in these outlying areas than in other parts of the country. Housing is predominantly singlefamily houses, most of which are relatively large and of high standard. 2.3.10 AgricultureUntil the end of the nineteenth century, farming was the Faroe Islands main industry, but with the economic and industrial development since then, particularly within fisheries, farming today accounts for only 0.7% of the Faroe Islands gross national income at factor cost. With a view to increasing the selfsufficiency of the Faroe Islands, the government is providing grants for investments in farming. With about 5% of the land under cultivation, the Faroe Islands can supply just over half of its total demand for lamb and mutton, most of its demand of milk, a fraction of its demand for beef and eggs, and half of the demand for potatoes. In 2001 the Faroe Islands had 1,170 dairy cows and about 70,000 sheep. 2.3.11 ForestryThere is no commercial forestry on the Faroe Islands, but there are a number of plantations on the islands, which are maintained by the Faroese forestry authority.
3 Greenhouse gas inventory information3.1 Greenhouse gas inventoriesDenmarks greenhouse gas inventories are prepared in accordance with the guidelines from the Intergovernmental Panel on Climate Change (IPCC) and are based on methods developed under the European CORINAIR programme (COordination of INformation on AIR emissions) for calculating national inventories1. The inventories follow the method described in CORINAIRs guidelines2 and IPCCs guidelines3. However, in accordance with the latter guidelines, the methods and emission factors have been modified for some of the inventories so that they reflect better Danish conditions. A description of methods, emission factors and activity data is given in Denmarks national emission inventory reports (NIR)4 to the Climate Convention. For the last two years these reports have included data in the common reporting format(CRF). The latest NIR and the latest combined Danish inventory of greenhouse gases and other air pollutants can be seen at the National Environmental Research Institutes website5 and in Illerup et al., 2002. Preliminary greenhouse gas inventories, for Greenland and the Faroe Islands are included in the annual inventory report to the Climate Convention. 3.2 Denmarks emissions and removals of greenhouse gasesDenmarks emissions of the greenhouse gases CO2 (carbon dioxide), CH4 (methane), N2O (nitrous oxide) and the so-called industrial gases, which include HFCs (hydrofluorocarbons), PFCs (perfluorocarbons) and SF6 (sulphur hexafluoride), for the period 1990 to 2001 are shown in tables 3.1-3.4 broken down into IPCCs six main categories and the most relevant sub-categories. The total emissions of these greenhouse gases, calculated in CO2 equivalents on the basis of the individual gases global warming potential, is shown in table 3.5. The development 1990-2001, broken down by source in table 10 in the reporting format CRF reported in NIR 2002, is reproduced in Annex A. 3.2.1 Carbon dioxide (CO2)Almost all the CO2 emissions come from combustion of coal, oil and natural gas at power stations and in residential properties and industry, although road traffic also accounts for a considerable part of it. The relatively large fluctuations in the emissions from year to year is due to trade in electricity with other countries mainly the Nordic countries. The large emissions in 1991 and 1996 resulted from large electricity exports. From 1990 to 1996, emissions showed a rising trend, but they have fallen since 1997 because many power stations have changed their fuel mix from coal to natural gas and renewable energy. As a result of the reduced use of coal in the last years, most of the CO2 emissions now come from combustion of oil. Emissions from road transport in 2001 accounted for more than 20% of the total CO2 emissions. Table 3.1: Table 3.2: The man-made emissions of methane (CH4) come from agriculture, landfill sites and energy production, with agriculture by far the largest source. The emissions from agriculture are due to the formation of methane in the digestive system of farm animals and due to treatment of manure. The methane emissions from landfill sites are falling because the amount of waste deposited is decreasing year by year as a consequence of the abrupt fall in the quantity of landfilled waste that has occurred since 1997. The emissions from energy production are rising because gas engines account for an increasing proportion. Gas engines have large emissions of methane compared with other combustion technologies. Table 3.3:Trend in N2O emissions 1990 - 2001 Agriculture is by far the biggest source of emissions of nitrous oxide (N2O) because this gas forms in soil during bacterial conversion of nitrogen in fertiliser and manure. Bacterial conversion of nitrogen also occurs in drain water and coastal water. This nitrogen largely comes from agricultures use of fertiliser, and emissions from these sources are therefore included under agriculture. It will be seen from table 3.3 that there has been a considerable fall in N2O emissions from agriculture since 1990. This is due to less and better use of fertiliser. A small part of the N2O emissions comes from the exhaust from cars fitted with a catalyser. Table 3.4:Trend in HFC, PFC and SF6 emissions 1990 - 2001
Source: National Environmental Research Institute Table 3.5: 3.2.4 The industrial gases HFCs, PFCs and SF6 The contribution of industrial greenhouse gases (HFCs, PFCs and SF6) to Denmarks total emissions of greenhouse gases is relatively modest, but has shown the strongest percentage rise during the 1990s. The HFCs, which are primarily used within the cooling industry, contribute most to the industrial greenhouse gas emissions. In the period 1990 to 2001, HFC emissions rose from 0 tonnes to 647,000 tonnes CO2 equivalents. There has been a relatively small increase and decrease in PFC emissions, while SF6 emissions have fallen considerably in the last few years.
Figure 3.1: Source: National Environmental Research Institute
Figure 3.2 Source: National Environmental Research Institute Table 3.6. 3.2.5 Denmarks total emissions and removals of greenhouse gases Table 3.5, figure 3.1 and figure 3.2 show the trend in Denmarks emissions and removals of greenhouse gases, given in CO2 equivalents and broken down into gases and sources in accordance with the general rules for inventories under the Climate Convention. CO2 is the main greenhouse gas, followed by N2O and CH4. It will be seen that there was a general fall in these emissions from 1996, when total emissions were (excluding LUCF) 90.8 million tonnes CO2 equivalents, to 2000, with total emissions of 68.1 million tonnes CO2 equivalents, while the total emissions in 2001 were 69.3 million tonnes CO2 equivalents. Of the total greenhouse gas emissions in CO2 equivalents, CO2 accounted for 78%, methane for 8%, nitrous oxide for 13% and the industrial gases HFCs, PFCs and SF6 for 1% in 2001. After deduction of the CO2 removals in forests, the total net Danish greenhouse gas emissions were 65.9 million tonnes CO2 equivalents in 2001. As will be seen from section 3.4, an inventory based on the rules under the Kyoto Protocol means certain changes with respect to base year and removals in connection with land-in-use change and forestry (LUCF). 3.3 Denmarks, Greenlands and the Faroe Islands total emissions and removals of greenhouse gasesThe total inventories for Denmark, Greenland and the Faroe Islands (the Kingdom) are given in table 3.6. As will be seen, the Climate Conventions goal of getting the level in 2000 down to the 1990 level was achieved. In 2000, the total level for Denmark, Greenland and the Faroe Islands lay 1.1% below the 1990 level. For the time being, the inventories from Greenland contain only inventories of the CO2 emissions from combustion of fossil fuels, which must, however, be regarded as by far the most important source of greenhouses gases. The inventories from the Faroe Islands include both an inventory of CO2 emissions from combustion of fossil fuels and inventories of methane and nitrous oxide emissions from agriculture. As will be seen from the table, Greenlands and the Faroe Islands greenhouse gas emissions are small compared with those of Denmark (each about 1% of the total emissions), and they have been almost constant since 1990. The sudden rise in CO2 emissions in the Faroe Islands in 1999 was due to a relatively big rise in imports of coal briquettes, while a similar rise in Greenland was due to increased sales of arctic gas oil in the towns. 3.4 Preliminary inventories under the Kyoto Protocol and the EUs burden-sharingIn sections 3.2 and 3.3, Denmarks, Greenlands and the Faroe Islands emissions and removals of greenhouse gases are calculated in accordance with the guidelines under the Climate Convention. Since the rules for inventories under the Kyoto Protocol differ on some points from the rules under the Convention, preliminary inventories are also made in accordance with the rules of the Protocol with a view to following the trend in relation to the obligation under the Protocol. In accordance with the rules of the Protocol, Denmark has chosen 1995 as the base year for industrial greenhouse gases (HFCs, PFCs and SF6), and, for the time being, the calculation under the Protocol includes only the removals occurring in forests as a consequence of afforestation since 1990. Denmarks reduction obligation is related to the EU reduction obligation through the so-called burden-sharing agreement. The Faroe Islands are not covered by the Kyoto Protocol since territorial reservation was made in connection with Denmarks ratification of the Protocol6. It was a condition of agreement by Denmark to a reduction contribution of 21% to the EUs total reduction obligation of 8% from 1990 to 2008- 2012 that account be taken of Denmarks relatively large electricity import in 1990 by adjusting CO2 emissions in 1990 so that these corresponded to the national energy consumption. It can thus be seen from Denmarks declaration, given in connection with, that the basis for the 21% reduction contribution has been adjusted. In connection with the EU ratification of the Kyoto Protocol, Denmark gave a legal undertaking to deliver a 21% reduction on the basis of the actual emissions level in 1990. The Council decision on the EUs ratification of the Protocol also refers to the fact that, in connection with the signing of the EUs agreement on the distribution of burdens in June 1998, certain Member States presented assumptions concerning emissions in the base year and common and coordinated policies and measures. In June 1998, Denmark was the only country to present a declaration with written assumptions concerning the base year. In connection with the decision on ratification by the EU, the Council and the Commission agreed on a joint declaration. This stated, inter alia, that the permitted emission levels (measured in tonnes CO2 equivalents) for the period 2008-2012 should be set taking account of the assumptions concerning emissions in the base year that also appear in the relevant declarations made in connection with the signing of the agreement on the distribution of burdens in June 1998. The permitted emission levels (measured in tonnes) are to be set not later than 2006. The setting of emission levels for the Member States will not affect the EUs total reduction target of 8% measured in tonnes. Table 3.7 shows the trend in Denmarks emissions and removals under the Kyoto Protocol in relation to the goal of a 21% reduction from the base year (1990/95) to 2008-2012, which Denmark has given a legal undertaking to achieve. To show the importance of the above-mentioned reference and declarations, table 3.7 also shows the trend in relation to a base year in which the CO2 emissions in 1990 are adjusted for electricity imports. Table 3.7. As far as is known, the trend in Greenlands emissions, calculated under the Kyoto Protocol,does not differ from the preliminary inventories of CO2 from use of energy calculated under the Climate Convention and appearing in table 3.6. The preliminary inventories form the basis for Denmarks climate strategy, as described in chapter 4.
4 Policies and measures4.1 Climate policy and the decision-making processSince the Brundtland Commissions report "Our Common Future" from 1987, Denmarks climate policy has been developed in interaction with the different sectors of society, international climate policy and the results of related research. Since the end of the 1980s many initiatives have been taken to reduce the emissions of greenhouse gases. The initiatives have produced important results particularly with respect to CO2 and will lead to further reductions in the emissions of greenhouse gases in the future. The initiatives have been and still are directed primarily towards the sectors of society whose activities are connected with considerable emissions of greenhouse gases. The initiatives have the objective of broad environmental improvements in society and include environmental taxes and involvement of the population in the debate and the decisionmaking process in the environmental field. A new objective is to ensure cost-effective action in order to achieve more environment for the money. In order to monitor the development of the overall effect of the initiatives on the emissions of greenhouse gases from energy consumption in Denmark, the basis for and follow-up on Denmarks action to reduce the emissions include emission inventories that are adjusted for inter-annual temperature variations and variations in Denmarks import/export of electricity . International climate objectives Since 1990 Denmark has undertaken or committed itself to several targets with respect to reducing greenhouse gas emissions:
Section 4.1.1 gives a short description of the general, democratic decision-making processes, to which Denmarks climate policy is also subject. In 1988 the government of that time issued "The Governments Action Plan for Environment and Development". The plan was a follow-up on the Brundtland Report and was based in principle on striving for environmentally sustainable development. One of the main messages in the plan was the need to integrate environmental considerations in decisions and administration within such sectors as transport, agriculture and energy. In the years since then a number of ministries have prepared sector action plans in which environment is an integral element. The sector action plans thus deal with the entire development in a sector combined with solutions of environmental problems caused by the sector. The sector plans for energy, transport, forestry, agriculture, aquatic environment, waste, and development assistance are important examples. The plans from the 1990s all contained specific environmental objectives and, usually, deadlines for a hieving them. In addition, there were a number of concrete initiatives that are intended to lead to achievement of the objectives. Progress has been evaluated regularly to check whether the implementation of the plans resulted in achievement of the objectives. The results of the evaluations have been presented in political reports from the sector ministries or in special follow-up reports. The evaluations and follow-up have often given rise to the preparation of new action plans, either because additional initiatives have been necessary in order to achieve the objectives or because the development of society or the development within the area in question has made it necessary to change both objectives and initiatives. Major sector plans that have been of importance for the reduction of greenhouse gas emissions are:
The sector plans deal with different aspects of the climate problem. In the energy and transport sectors the main environmental concern has been the emissions of the greenhouse gas CO2. The plans in these sectors were therefore to a great extent concerned with reducing CO2. The other sector plans are not primarily focused on reducing greenhouse gas emissions, in part because the sectors are battling with other major environmental problems that efforts have been made to solve through the plans. The main concern in the agricultural sector has been pollution of the aquatic environment. In the waste sector it has been reduction of the volume of waste, and in the industrial sector, reduction of emissions/discharges of harmful substances to the atmosphere/aquatic environment, the use of toxic substances, etc. However, the implementation of the sector plans has to a great extent also resulted in reduction of greenhouse gas emissions. For example, the reduction in the agricultural sectors nitrogen emissions, which the aquatic environment plans are resulting in, is at the same time reducing the emissions of the greenhouse gas nitrous oxide. The initiatives to reduce waste quantities mean fewer landfill sites and thus less formation and emissions of methane, and the ongoing increase in forested area will mean increased removals of CO2. In addition, the energy and transport plans meant that changes were made in the energy and transport areas in all sectors. The initiatives in the energy area have thus resulted in reduced energy consumption and, with that, reduced CO2 emissions within a wide range of sectors, including the domestic sector and the business sector. In June 2002 the governments national strategy for sustainable development in Denmark, "A SHARED FUTURE balanced development" was adopted by the Folketing. The strategy must be seen in part as one of Denmarks responses to the challenge of Agenda 21, which was adopted at the UN General Assembly in Rio in 1992. The government lists eight objectives and principles for creating sustainable development:
The strategy is built up with a number of sectors: food production, forestry, industry, transport, energy, urban and housing development, and intersectoral action: climate change, biodiversity, environment and health, resources and resource efficiency, knowledge and policies and measures, the global dimension and public participation. In order to follow developments in relation to the strategy, regular indicator reports are prepared. The first, from August 2002, contains 14 key indicators including indicators for economic growth, greenhouse gas emissions, air pollution, employment and discharge of nutrients to the marine environment. In addition, the trend in a wide range of more specific indicators is being monitored. Examples of these indicators are the l ng term development in average temperatures near ground level globally and in Denmark, the beginning and the size of the pollen season, the incidence of asthma, the thickness of the ozone layer, by-catches of porpoises, the amount of PCB in cod liver and the number of organic farms. The conclusion of the indicator report is that Denmark is on the way to sustainable development since the indicators show that Denmarks stable economic growth has happened without corresponding increases in a number of environmental parameters. For example that energy consumption and greenhouse gas emissionss have not risen in step with the economy, and that the consumption of drinking water and discharges of acid substances have fallen. On the environment policy front, Denmark has participated actively in improving environmental protection in Europe through the EU cooperation and through bilateral environmental assistance to Central and Eastern European countries. On a number of points, the EUs environmental regulation has put Europe ahead of the rest of world environmentally. There are also many examples of EU rules having helped to strengthen environmental protection in Denmark. With the adoption of the Amsterdam Treaty, sustainable development became a main objective for the EU, and integrating environmental considerations in the EUs sector policies became an obligation. 4.1.2 Denmarks new climate strategy In February 2003 the government published Denmarks new climate strategy. The basis of the strategy is that Denmark must fulfil its international climate obligations following from the Kyoto Protocol and the subsequent EU burden sharing agreement. Although many important initiatives have already been launched in order to live up to the climate objective, considerable work still remains before Denmark can live up to its very ambitious Kyoto objective. According to the latest projection of Denmarks emissions of greenhouse gases1, it is estimated that, unless additional measures are initiated, Denmark will be 20-252 million tonnes CO2 equivalents per year short of achieving its reduction obligation under the Kyoto Protocol in the period 2008-2012. It is therefore vital in the climate strategy to plan the action cost-effectively. The Kyoto Protocol offers the possibility of planning climate action that is more flexible and that, globally, gives more environment for the money. The climate strategy combines cost-effective national measures with use of the Kyoto Protocols flexible mechanisms. For many of Denmarks energy producers and a large part of the energy- intensive industry, the coming EU Directive on a scheme for trading with greenhouse gas emissions within the Community will form the framework for the coming action. The companies that will be covered by the scheme, and whose activity will be regulated by a quota, will be able to plan their climate action themselves. They can choose to reduce their own emissions when that is most appropriate or to buy quotas or credits from project-based emission reductions when that is deemed most suitable. This means that the companies concerned will be able to adjust their action on an ongoing basis so that it is always as effective as possible. Reduction is primarily a task for the private sector, but government action can supplement the private sector action and, in the start-up phase, help to get the market for CO2 credits going. Besides quota management and use of flexible mechanisms, the climate strategy includes a number of national measures, including initiatives to promote continued energy savings and improve of energy efficiency. Within the agricultural sector there may also be possibilities for reducing greenhouse gas emissions. However, the potential has not been sufficiently clarified at the present time, and the possibilities for additional cost-effective measures within this sector willbe analysed in connection with a coming Action Plan for the Aquatic Environment III. Within transport the selected analyses carried out show that national solutions for the most part are relatively expensive. However, it is estimated that more efficient and less expensive initiatives may be carried out jointly at EU level. Since the reduction costs in the different sectors are constantly changing as a consequence of technological development and changed economic framework conditions, the strategy includes regular evaluation of the action in order to ensure that the most cost-effective policies and measures are chosen. 4.1.3 Economic aspects of the climate policy The picture of potentials and economic reductions in costs that can be given at the present time for selected national measures to reduce greenhouse gas emissions are shown in table 4.1. Table 4.1
In a comparison with the national policies and measures, it is important to be aware that these must typically be seen in a sector-political context, in which climate is just one of many considerations in the policy planned. For example, a fundamental consideration in the energy sector is security of supply, which, all else being equal, is improved by a lower energy consumption and a diversified energy supply. The analyses carried out do not cover every conceivable national measure, and the costs may change in the coming years as a consequence of new knowledge and new technologies. An interministerial committee will regularly evaluate the costeffectiveness of the national policies and measures, including new ones that are not mentioned in table 4.1. The government has set an economic marker of DKK 120/tonne CO2 equivalents to be used as a basis for implementing national policies and measures outside the area covered by the EU trading scheme. The analyses show that only relatively few national policies and measures with a significant potential, that do not exceed DKK 120/tonne CO2 equivalents, would be able to compete with the price of using the flexible mechanisms. This must be seen in the light of the fact that Denmark has already made a massive national effort up through the 1990s, while there is a large, unexploited potential in other countries. For the national policies and measures, where the analyses show relatively low reduction costs, the potential is, all in all, insufficient to meet the need for making up the Danish reduction shortfall. On the other hand, there is considered to be a considerable potential for buying quotas and credits internationally. For these reasons, the government's cost-effective strategy for meeting Denmark's reduction obligation is to a certain extent based on the use of flexible mechanisms - emissions trading and the project mechanisms, Joint Implementation and the Clean Development Mechanism. The EU trading scheme will be a key instrument. The actual composition of the action will therefore depend on the extent to which the companies concerned choose to implement their own reduction measures or to buy quotas abroad. Table 4.2
Table 4.3 4.2 Policies and measures and their effects in Denmark's economic sectorsIn sections 4.2.1 to 4.2.6 below, policies and measures of importance for emissions and removals of greenhouse gases are examined within the following six economic sectors: energy, transport, the business sector, agriculture and forestry, the domestic sector and waste. Table 4.2 shows how the sector classification that is to be used in connection with the annual emission inventories (the CRF/IPCC format) is aggregated to the six economic sectors. Table 4.3 shows the main result of this aggregation for the base year, 2001, 2008-2012 and 2013-2017.
Figure 4.1 Source: National Environmental Research Institute and the Danish Environmental Protection Agency 4.2.1 EnergyThe energy sector's production, conversion, and distribution of energy account for 40% of Denmark's total greenhouse gas emissions, and mainly the greenhouse gas CO2 is emitted. 97% of the total greenhouse gas emissions from the energy sector is CO2, 2% is methane (CH4) and 1% is nitrous oxide (N2O). CO2 Energy production and energyconsuming activities in the transport sector, industry and the other sectors are the main contributors to the total emissions of CO2 due to use of large quantities of coal, oil and natural gas. The energy sector is therefore centrally placed in the efforts to reduce the emissions of CO2. Many initiatives have been taken over the years to reduce the emissions, and work is still going on to find the best and most cost-effective measures with a view to fulfilling Denmark's international climate obligations. The focus of this section is energy production and energy supply. The energy-consuming activities and the possibilities for energy savings in the different sectors of society are dealt with in greater detail in the subsequent sections. Implemented policies and measures Some policies and measures can bring general pressure to bear on players in the energy sector to get them to reduce their CO2 emissions. Denmark's national Quota Act, which regulates the emissions of CO2 from open, market-regulated production of electricity is an example. The CO2 Quota Act puts a ceiling on the electricity producers' CO2 emissions. If the producers exceed a set quota, a penalty tax is imposed on them for every tonne by which the quota is exceeded. The producers can decide for themselves how they keep to the quota - whether by energy efficiency improvements at their plants, by changes in fuel or by reducing production. The Danish producers can also trade quotas among themselves. Taxes have also been used for many years as an instrument for reducing the CO2 emissions from the energy sector, since fuels used for heat production have been subject to a CO2 tax and an energy tax for many years, partly with a view to a general reduction in energy consumption and partly to promote fuels with lower CO2 emissions - primarily biomass, on which there is no CO2 tax and, in the case of most applications, no energy taxes either. R&D activities include energy savings, more efficient energy conversion and renewable energy technologies. Table 4.4
Use of renewable energy sources can reduce the emissions of CO2 from fossil fuels. The proportion of Denmark's gross energy consumption that is covered by renewable energy increased from 6.5% in 1990 to 12% in 2001 and is expected to reach about 14% in 2010. Renewable energy sources are promoted through economic instruments, including the tax system, and by direct production or establishment grants. Contracts and orders within the electricity and heat sector used to play a role, but use of this instrument has largely ended. Lastly, financing R&D activities is contributing to the continued growth in the proportion of renewable energy. Substitution of natural gas for coal or oil reduces the emissions of CO2. The first Danish natural gas was landed from the Danish sector of the North Sea in 1984. From then, natural gas consumption increased to 193 PJ in 2001 and accounted for 23% of gross energy consumption. Growth is now expected to stop, in part because of the relative high price of natural gas. Natural gas is favoured by a lower CO2 tax than oil and coal because of its lower emissions and will be promoted by the coming EU trading scheme. The ongoing liberalisation of the Danish natural gas sector may also result in lower prices and thus increased use of natural gas. Additional policies and measures With the energy sector's big contribution to Denmark's total emissions of greenhouse gases, action in the energy sector is an absolutely vital element of Denmark's new climate strategy. In particular, it is estimated that expected rising electricity exports could result in a considerable increase in emissions if measures are not taken to prevent this. Electricity production is covered by the proposed EU Directive on emissions trading. The climate strategy is based on the assumption that electricity production will be covered by the EU's scheme from 2005. Since all the EU Member States' electricity producers will be subject to quotas on their fossil electricity production, electricity prices are expected to rise across Europe. That offers the possibility of imposing rather tight CO2 quotas on the electricity producers so that Denmark's fulfilment of the climate objective is not affected by any high electricity export. In periods with high electricity prices, electricity producers are expected to make considerable use of the flexible mechanisms. The existing national CO2 quota regulation of electricity production ends at the end of 2003. The heat sector is today subject to full CO2 and energy taxes and is also subject to considerable administrative regulation. In connection with the climate strategy it is therefore believed that there is limited room for further cost-effective reduction measures. In the climate strategy it is proposed that the sector be kept outside the quota regulation for the first period, 2005-2007. After that, according to the present proposal for a trading directive, this sector will also be covered by quota regulation. Methane, CH4 Many small sources contribute to the energy sector's methane emissions. The biggest single contribution comes from gas-fired CHP plants, which emit uncombusted natural gas. With a view to minimising the emissions, a statutory order now limits the emissions from new plants, corresponding to about 3% of fuel consumption. 4.2.2 TransportIn 2001 the transport sector accounted for 18% of Denmark's total emissions of greenhouse gases. Of the transport sector's emissions, CO2 accounts for 96%, corresponding to 12 million tonnes of CO2, nitrous oxide for 3% or 395,000 tonnes of CO2 equivalents, and methane for about 1%, corresponding to 70,000 tonnes CO2 equivalents. In 2001 the transport sector's energy consumption - mainly oil products - accounted for about 30% of energy consumption in Denmark. Traffic, particularly passenger traffic, has increased steadily in the last few years. In step with the increase, energy consumption and greenhouse gas emissions have also increased. In 2001 greenhouse gas emissions from the transport sector were 17% above the 1990 level. The latest forecast from 2002 indicates that, without additional initiatives, the sector's emissions in 2005 will be 24% above the 1990 level, rising to about 35% in the first commitment period 2008-2012. CO2 Efforts to curb the upward trend of greenhouse gas emissions in the transport sector have not yet succeeded, in part because reducing CO2 emissions in Denmark, which is not a car manufacturing country, is extremely difficult without international initiatives. As shown in table 4.2, the greenhouse gas emissions from fuel for vehicles, ships and aircraft are included under transport. The contribution from the armed forces consists mainly of CO2 and accounts for just under 2% of the inventory for the transport sector. The proportion of fuel consumption for multilateral military operations, which is therefore kept out of the total national inventory, is at present regarded as minimal. Implemented policies and measures In 2002, working on the basis of the previous trends in passenger and freight traffic, the Danish Road Directorate carried out a projection of road traffic up to 2016. The projection indicates that road traffic will continue to grow. With the chosen assumptions it is estimated that road traffic will grow by more than 25% from 1997 to 2016. In the period 2000 to 2010, growth is expected to lie at about 13%. A large part of total freight and passenger transport is by road and is expected to increase. The trend in freight and passenger transport by road will therefore determine the transport sector's energy consumption and thus its CO2 emissions. Table 4.5 shows the existing policies and measures within the transport sector. In the last few years a number of important steps have been taken at international level, and these - supported by targeted and effective Danish action may help to turn the trend for the transport sector's CO2 emissions. Additional policies and measures The transport sector's possibilities for contribution to reduction of Denmark's CO2 emissions show that the cost-effectiveness of the measures is totally dependent on the sideeffects, cf. table 4.1. The decision to implement the various measures within the transport sector must therefore be evaluated on the basis of the measures' other effects and not from a pure CO2 consideration. The generally high economic shadow prices without side-effects are primarily a consequence of the already high level of taxation in the transport sector. It is thus a common feature of most of the measures that they are directed towards parts of the transport sector that, taken together, pay the full economic cost of transport, since there is a considerable fiscal element in the regular car taxes. Methane, CH4 The transport sector's emissions of methane account for about 1% of the sector's greenhouse gas emissions, corresponding to about 70,000 tonnes CO2 equivalents. Nitrous oxide, N2O Nitrous oxide accounts for 3% of the transport sector's total greenhouse gas emissions, or 380,000 tonnes CO2 equivalents. 4.2.3 Business sectorThe business sector covers industry, building and construction and public and private service. The sector accounts for about 13% of Denmark's total greenhouse gas emissions. By far the largest part, 93%, is CO2. The sector is also the only source of emissions of industrial gases. Table 4.6 shows the policies and measures within the business sector. Table 4.5
Table 4.6
Earlier analyses have shown that there is a big potential for profitable energy efficiency improvements within the business sector, so improving energy efficiency is a vital area of action. CO2 Industry, building and construction, trade and private service Industry is responsible for most of the sectors' emissions of CO2. The emissions come mainly from energyconsuming activities in industry. Cement and brick production also contributes CO2, which comes from the raw materials used. The main measure used to get the business sector's energy consumption down is a green tax package for the business sector, which was introduced in 1995. The package contained a combination of taxes and return of the proceeds to businesses through government grants etc. to promote energy savings in companies. The package led to a higher CO2 tax and the introduction of a space-heating tax for businesses. At the same time, a scheme was introduced in which companies with a big energy consumption have the possibility of gaining a discount on the taxes in return for entering into an agreement on energy efficiency improvements. The combination of taxes and return of the proceeds was intended to ensure a marked reduction of businesses' CO2 without affecting their international competitiveness. The grants were also intended to promote the use of more energyefficient technologies and production methods. The objective with the green tax package was to get the business sector to contribute to a reduction of Denmark's total CO2 emissions. The target contribution was about 4% in 2005 in relation to the emissions in 1988. The green package's overall effect was evaluated in 1999. The main conclusion is that the package has functioned as intended. Considerable environmental gains have been achieved in an economically effective way that takes account of businesses' international competitiveness. The energy package's environmental effects largely live up to the original expectations and the package is thus an important element of the efforts to reduce Denmark's CO2 emissions. In the climate strategy from February 2003 it was evaluated whether there was still a potential for relatively cheap emission reductions in the energy-intensive part of industry, which had hitherto paid lower CO2 taxes than the rest of the business sector and the domestic sector for reasons of competitiveness. With a common EU trading scheme, some energy-intensive companies could be made subject to tighter CO2 regulation than hitherto without affecting their competitiveness too seriously. For these companies future regulation is thus expected to be based on implementation of the common EU trading scheme. This also applies to the product emissions that do not come from energy consumption but that are covered by the EU trading scheme. In Denmark's case, it will be primarily the CO2 emissions from cement production. These emissions have not previously been regulated. CO2 emissions from public service Data on energy consumption in the public sector have been collected for some years as a means of rendering the sector's energy consumption visible. As a consequence there are now complete inventories of energy consumption in county and state institutions, but more limited inventories of the individual municipalities' energy consumption. The main initiatives to promote energy savings in the public sector are:
Work on improving energy efficiency in the public sector has now been going on for more than 10 years, and considerable savings have been achieved. However, there are still economically profitable possibilities for savings. This is illustrated by the fact that there is a very big difference in consumption (per m2) between comparable institutions. In continuation of the provisions in the Act on Promotion of Savings in Energy Consumption from 2000 and several energy policy agreements, plans are in hand for further tightening, particularly in the state sector. The circular's requirements will be tightened and so will the obligation concerning energy-afficient procurement. CO2 emissions from cement production Cement production results in big emissions of CO2. The production process itself is very energyintensive and, a large quantity of CO2 is emitted in connection with the process. It takes about 4,950 MJ energy to produce 1 tonne of cement. Cement production in Denmark is concentrated in a single company. In 2001 the total annual emissions of CO2 from cement production were about 2.6 million tonnes. About half comes from energy consumption and the other half from chalk, which is one of the raw materials used in the process. A lot has been done within the cement industry. For example, in the last 20 years the Danish cement producer has reduced its CO2 emissions by about 13% per tonne cement produced. In addition, cooperation with the Danish Environmental Protection Agency is expected to result in increased use of alternative fuels,which will reduce the CO2 emissions still further. The action on the cement industry's energy consumption has also hitherto been based on the green tax package for businesses, with a combination of taxes and agreements on energy efficiency improvements. In future, regulation of the industry's energy consumption will be based on implementation of the EU emissions trading scheme. As mentioned earlier, this will also apply to product emissions that do not come from energy consumption. HFCs, PFCs and SF6 The industrial sector is the only sector with emissions of the industrial gases HFCs, PFCs and SF6. These gases are used as cooling and foaming agents etc. (HFCs), cooling agents (PFCs) and as insulating gas in high voltage contacts and as noisedamping gas in thermal glazing (SF6). The emissions of the industrial greenhouse gases (HFCs, PFCs and SF6) are regulated in two ways - partly by a tax and partly by a statutory order on discontinuation of use of the gases in new installations. Since 1 March 2001 a tax has been payable on the industrial greenhouse gases corresponding to their GWP, combined with the Danish CO2 tax of DKK 0.1/kg CO2. This means that HFC-134a is subject to a tax of DKK 130/kg because it has a GWP of 1,300. There is a ceiling of DKK 400/kg so although SF6 has a GWP of 23,900, the tax is only DKK 400/kg and not DKK 2,300/kg. The tax is imposed on the substances on importation into Denmark because the substances are not produced in Denmark. The tax is payable whether the substances are imported as pure substances or are part of imported products. If the content in the products is not known, the tax is based on a fixed tariff. The tax is payable on a wide range of products, including:
Table 4.7
In the spring of 2002 the Danish government issueda revised draft of a statutory order regulating the industrial greenhouse gases for national consultation. A first draft had been sent for notification in the EU in February 2001. The final statutory order entered into force on 15 July 2002. The regulation includes a general ban on use of the industrial greenhouse gases in a wide range of new installations/products from 1 January 2006, including, for example, domestic refrigerators and freezers, PUR foam, etc. There are certain exceptions from the date for the general ban. For example, the ban will only apply to new commercial cooling plants, air-conditioning plants, etc. from 1 January 2007. Other exceptions are new sound-insulating windows, in which SF6 has been banned since 1 January 2003, and PFCs, on which there has been a general ban since September 2002. However, some products and applications are exempted from the ban. This applies, for example, to service on existing plants, mobile cooling plants, including mobile air conditioning plants, cooling and air conditioning plants with HFC fillings between 0.150 and 10 kg HFC, electric switches, etc. 4.2.4 Agriculture, forestry and fisheriesThe sectors agriculture, forestry and fisheries are generally considered as one single economic sector in Denmark. However, the importance of the individual sectors differs greatly with respect to Denmark's emissions and uptake of greenhouse gases. Agricultural farms have emissions of methane and nitrous oxide. The net uptake of CO2 in Denmark's forests is included under Forestry. However, CO2 emissions from energy use in all three sectors are considered under one heading because there is no breakdown of these in the annual energy statistics. Table 4.7 shows policies and measures for emission reductions within agriculture and forestry. In 2001 agriculture accounted for 20% of Denmark's total greenhouse gas emissions, which consists mainly of methane and nitrous oxide, while a smaller percentage is CO2. Measures that are used in the agricultural sector and that have affected or will affect the sector's greenhouse gas emissions include:
Methane, CH4 Methane comes mainly from the agricultural sector. The emissions in 2001 were 173,000 tonnes, corresponding to 3.6 million tonnes CO2 equivalents. The methane is formed through enteric fermentation in farm animals and from conversion of carbohydrates in manure. Agriculture's biggest contribution to the methane emissions comes from dairy cows. In the digestion process, methane is a by-product of the fermentation of feed in the rumen, primarily from grass and green fodder. In addition, methane formed during conversion of manure under anaerobic conditiions if the temperature is sufficiently high. These conditions normally occur in manure stores and housing systems with liquid manure or deep litter. Methane emissions within agriculture are expected to fall by about 0.4 million tonnes CO2 equivalents from 2001 to 2012 due to continued efficiency improvements in cattle farming and, to a lesser extent, to more biogas plants. Nitrous oxide, N2O Agriculture is the biggest source of nitrous oxide emissions in Denmark. Of the total emissions of 28,200 tonnes in 2001, 25,500 tonnes or 91% came from agriculture. The nitrous oxide emissions from agriculture correspond to more than 8.0 million tonnes CO2 equivalents. Nitrous oxide may be emitted during microbial decomposition of organic matter. The process occurs in some types of manure stores and during conversion of minerally and organically bound nitrogen (e.g. manure and applied wastewater sludge) in the soil. Some of the leached nitrogen is also converted into nitrous oxide. Nitrogen entering the soil with fertiliser and manure and in plant residues is the main cause of nitrous gas emissions. In 2000 agriculture's main contribution to the nitrous oxide emissions consisted of a contribution of 40% from manure and a contribution of 26% from leaching3. Ammonia volatilization contributes to the greenhouse effect because some of the ammonia nitrate ends up as nitrous oxide in the atmosphere. Ammonia volatilization into the atmosphere comes almost exclusively from agriculture. In 2000 the NH3-N emissions from agriculture were slightly more than 84,000 tonnes, with a nitrous oxide contribution corresponding to 4% of agriculture's nitrous oxide emissions4. Ammonia volatilizes from manure, fertiliser, sludge, crops and treatment of straw with ammonia. The emissions occur during handling of manure in animal housing, during application of manure, and from grazing animals. Implemented policies and measures with effect on the N2O emissions Nitrous oxide emissions in agriculture are expected to fall by about 2.7 million tonnes CO2 equivalents, or 26%, in the period from 1990 to 2008-12. The implementation of the Action Plans for the Aquatic Environment will be the main contribution to this reduction. Action Plan for the Aquatic Environment I and II and Action Plan for Sustainable Agriculture One of the main purposes of Action Plan for the Aquatic Environment I and II and the Action Plan for Sustainable Agriculture was to reduce agriculture's emissions of nitrogen to the aquatic environment. The action plans have been implemented as regulation of farmers' behaviour. The Action Plan for the Aquatic Environment I was initiated in 1987 and The Action Plan for Sustainable Agriculture in 1991. These action plans included particularly requirements concerning winter green fields and better utilisation of manure. The Action Plan for the Aquatic Environment II from 1998 contained a number of additional measures, including re-establishment of wetlands, afforestation, agreements on Environment friendly Agricultural Measures, organic farming on an additional 170,000 ha, improved use of fodder, reduced animal density, use of catch crops, reduced fertilisation norms and stricter requirements concerning the use of nitrogen in manure. The aim was to reduce nitrogen leaching by 100,000 tonnes/year up to the year 20035. These action plans have, in particular, reduced the emissions of nitrous oxide. There have presumably also been small effects on methane emissions from manure stores, particularly as a consequence of increased use of anaerobic fermentation of manure in biogas plants. The increased use of catch crops, larger areas with organic farming and re-establishment of wetlands must also be expected to lead to increased storage of carbon in the soil. Most of the changes in nitrous oxide emissions from agriculture in the period since 1990 can be attributed to these action plans. On this basis, the reduction in nitrous oxide emissions can be calculated as 1.2 million tonnes CO2 equivalents/year in 1995, 1.8 million in 2000 and 2.7 million in 2005. There are no estimates of the effect on carbon storage in the soil. Ammonia Action Plan Ammonia emitted from agriculture will stimulate emissions of nitrous oxide when it is deposited in other ecosystems. Reducing ammonia evaporation will therefore also result in a reduction of nitrous oxide emissions. In 2001 an ammonia action plan was adopted. This, together with Action Plan for the Aquatic Environment I and II, will reduce ammonia volatilization by 15-20,000 tonnes N/year. This means that ammonia volatilization in agriculture should be reduced from about 90,000 tonnes N in the middle of the 1990s to about 75,000 tonnes N in 2004. The measures covered by the Ammonia Action Plan are:
It is estimated that these measures will together result in a reduction of nitrous oxide emissions corresponding to 34,000 tonnes CO2 equivalents/ year in 2010. Here, the shorter time from application to incorporation has the biggest effect - 13,000 tonnes CO2 equivalents/year6. Ban on burning of straw The purpose of the ban has been to reduce air pollution from burning of straw. The ban has resulted in more carbon being returned to the soil and greater use of straw as a fuel. Both uses will result in a net reduction in CO2 emissions. Not burning straw prevents the methane and nitrous oxide emissions associated with the burning. On the other hand, there are some emissions of nitrous oxide in connection with the return of nitrogen to the soil when the straw is mulched. The measure works by regulating behaviour, and the ban was introduced in 1989. The measure was implemented in the form of a statutory order under the Environmental Protection Act, and compliance is monitored by the local authorities. There are no estimates of the effect on greenhouse gas emissions. CO2 The green tax package and the grant scheme for energy savings in the business sector are resulting in energy savings and thus a reduction in CO2 emissions from use of energy in agriculture. Implemented policies and measures with effect on the emissions and the removals of CO2 The aim is to increase use of biomass for energy purposes by establishing power stations and CHP plants using this fuel. Straw as a fuel will substitute fossil fuels but will also reduce the amount of carbon returned to the soil. The latter may result in less carbon storage in the soil. At the same time, less nitrogen will be returned to the soil, which will mean a small reduction in nitrous gas emissions from the soil. In 1990, 720,000 tonnes of straw were used for energy purposes and, in 2000, 900,000 tonnes. However, the use of straw for energy purposes has negative impacts on carbon storage in the soil and presumably on the soil's fertility7. Compared with ordinary grain cultivation, it is calculated that cultivation of perennial energy crops corresponding to production of 5 PJ calorific value could reduce CO2 emissions by 285,000 tonnes/year from substitution of fossil energy, 75,000 tonnes/year from carbon storage in soil, 10,000 tonnes/year from energy saving in cultivation of the crops and 30,000 tonnes/year from reduced nitrous oxide emissions8. Forestry is important due to its CO2 sequestration and emissions being a consequence of trees growing, respiring and decomposing. An average Danish forest contains a considerable store of CO2 absorbed from the atmosphere. When new forests are established, new CO2 stores are created. Afforestation is therefore a useful climate policy instrument. Table 4.8 Calculating the total CO2 accumulation in forests is complicated. Almost all existing forests are established for wood production, e.g. logs and timber. Whether there are netemissions or net-sequestration of CO2 from an existing forest depends on many factors, including it's age and species distribution, and the management regime applied. Compared with other sectors, forestry has very low energy consumption. Green accounting and environmental management are being developed in the sector, partly with a view to determining whether the use of fossil fuels can be reduced. The national forest programme provides for considering the potential of establishing economic incentives for increasing CO2 sequestration in forests within the framework of the Kyoto Protocol. Such meausures should be implemented without undermining the Protocol's environmental integrity or counteracting established measures in support of sustainable forest management. The same should also apply to forest projects in connection with CDM and JI. The forests are managed with a view to multiple-use and sustainability, and carbon sequestration is one of several objectives. The policy objective most likely to increase carbon sequestration is the 1989 target to double Denmark's forested area within 100 years. There are several measures aiming at achieving this objective. Firstly, a government subsidy scheme has been established that supports private afforestation on agricultural land. Secondly, also state afforestation is taking place, and thirdly some private afforestation is taking place without subsidies. Primarily the CO2 balance is affected by these measures. Forests raised on agricultural land accumulate far more biomass than the previous agricultural land-use. The forest biomass contains about 50% carbon, which is absorbed as CO2 through photosynthesis. Probably, additional carbon is stored in the organic matter in the soil due to a larger supply of dead organic matter and the absence of soil preparation. The effect of afforestation on other greenhouse gases, such as nitrous oxide and methane has not been properly clarified. However, the acidification of nitrogen-rich former agricultural land may stimulate the formation of nitrous oxide, and blocking of drains after afforestation and the resulting water stagnation could increase methane emissions. Increased methane and nitrous oxide emissions could counteract the positive effect of afforestation on CO2 sequestration. However, since sufficient information is still unavailable on changes in the methane and nitrous oxide emissions, analyses of the consequences are only carried out for CO2. The Danish Forest and Nature Agency is responsible for policies on afforestation on private agricultural land and on state-owned land. Through 1990-2002 subsidies were provided for 11,000 ha of private afforestation on agricultural land, catering for an extra sequestration of 68,000 tonnes CO2. The cost of this afforestation was DKK 620 million. At a discount rate of 6%, the economic shadow price per tonne sequestered CO2 is DKK 641 without side-effects and DKK 566 with sideeffects. At a discount rate of 3%, the shadow price is DKK 303 without side-effects and DKK 237 with sideeffects. The side-effects of afforestaion are linked to recreational value, groundwater protection and other factors. The state, counties and municipalities have established about 5,500 ha of new forest since 1990. Only little is known about private afforestation without subsidies. It is assumed that about 600 ha are planted annually. The annual quantities of CO2 sequested as a consequence of subsidised private afforestation, public afforestation and the total afforestation are summed up in table 4.8. Carbon sequestration in trees after afforestation is calculated by a simple model. Sequestration is obtained as the planted area multiplied by the carbon absorption for the age class of the trees. The absorption is calculated by using Danish increment tables for Norway spruce, as representative of conifers, and oak, as representative of deciduous trees9. Table 4.9
The quantities of carbon are obtained by estimating the carbon content of the woody biomass using relevant conversion factors. The stem biomass for conifers and the total above-ground woody biomass for deciduous trees are converted into total aboveground and belowground biomass by multiplying with an expansion factor. An expansion factor of 2 is used, which is somewhat higher than the expansion factors used for forests planted before 1990 - 1.8 for conifers and 1.2 for deciduous trees. The reason for this is that the expansion factor depends on age. The stem biomass thus constitutes a very small part of the total biomass in entirely young trees. The expansion factor therefore decreases exponentially towards a value between 1 and 2 as the trees grow older13. Since there are neither Danish expansion factors nor agedependent expansion functions, the expansion factor of 2 is being used until better methodologies are available. The total biomass is subsequently converted into tonnes dry matter using the conversion factors 0.38 tonnes dry matter m-3 for conifers and 0.56 tonnes dry matter m-3 for deciduous trees14. The quantity of carbon is calculated by multiplying with the conversion factor 0.5 tonnes C/tonne dry matter. Carbon sequestration in products can be included in the calculations, but the figures presented represent only the quantity of carbon that is sequestered in the forest ecosystem. This quantity of carbon is stored in the total living biomass (incl. roots) of the trees and in slash. The quantity of sequestered carbon is summed by the model for the different year classes of afforested areas since 1990, providing the total carbon sequestration for the differently aged stands in specific years. Studies of soils in a time series of afforested stands have shown that, compared with the biomass carbon pool, there is no great change in the soil carbon pool during the first 30 years after afforestation15. It is assumed in the models that the growth of the trees correponds to site index 2 (on a scale decreasing from 1 to 4), and that there is a ratio of 1 to 3 between the area afforested with conifers and deciduous trees16. Afforestation offers many other benefits in addition to carbon sequestration. Besides being valuable for outdoor recreation it provides valuable ground water protection and protection of habitats for fauna and flora. Forest is also a highly valued type of nature in terms of cultural values and landscape amenity. In addition to carbon sequestration, afforestation thus contributes to a wide range of values. The above-mentioned shadow price for sequestration of carbon includes side-effects due to, for example, outdoor recreation. The continued growth of new forests will provide for carbon sequestration on a long-term basis. If the objective of doubling the Danish forested area within 100 years is achieved, the new forests will sequester about 250 million tonnes of CO2 over the next approximately 120 years. Owing to the legal protection of forest landuse, the sequestration will be permanent. If the objective of doubling the forest area is to be achieved, however, an enhanced rate of planting will be needed. Danish forest policy is moving towards more near-to-nature forest management. In the long term, this change will increase carbon sequestration in existing forests. The inventories of the total emissions and removals of greenhouse gases include the emissions of greenhouse gases from fuel sold for fishing vessels. The fishing vessels' contribution to greenhouse gas emissions consist primarily of CO2. No special initiatives have been put in place concerning this, but the reduction in the number of fishing vessels in recent years has also resulted in a reduction in fuel consumption and thus also in emissions of CO2. 4.2.5 Domestic sectorThe domestic sector's contribution to greenhouse gas emissions, which was 4.4 million tonnes CO2 equivalents in 2001, consists mainly of CO2 (97%). There are also small emissions of methane and even smaller emissions of nitrous oxide. CO2 The CO2 emissions come from households' energy consumption, which accounts for almost 30% of total energy consumption in Denmark. The largest part of the energy consumption is used for heating homes, where burning of oil and natural gas results in a CO2 emissions. A large part of the space heating is in the form of district heating (about 47%), which results in CO2 emissions in connection with the production of district heat. When district heat is produced at CHP plants or with CO2-friendly fuels, such as natural gas and, particularly, renewable energy, there are big savings overall from use of district heating instead of individual heating based on, for example, oil-fired boilers. CO2 emissions from the production of district heat are taken into account under the energy sector. Danish households also have a substantial consumption of electricity, which also means CO2 emissions from power stations. These emissions are taken into account under the energy sector. Most of the households' electricity consumption is used for electrical appliances and light sources, while just under 25% is used for electric heating. Consumption for electric heating has been decreasing in recent years as a consequence of the work of the Electricity Saving Trust, which has resulted in considerable conversion from electric heating to district heating and natural gas heating. Households' transport consumption also results in emissions of CO2. Unlike households' electricity and heat consumption, transport consumption is still increasing considerably. Households' disposal of waste also contributes to emissions of methane from landfill sites. The action being taken on households' waste and transport consumption is described in the sections on waste and transport. This section therefore concentrates on the possibilities of reducing the CO2 emissions through savings in electricity and heating in households and the possibilities for conversion to more environment-friendly forms of heating. The possibilities for reduction in the public energy supply system are described in the section on the energy sector. In 2001 the domestic sector used in all 156 PJ energy for space heating (climate adjusted) and 30 PJ electricity for appliances etc. The consumption for heating has been fairly constant for a number of years despite some growth in the number of households and increase in the area heated. Electricity consumption for appliances etc. has risen only slightly since the mid-1990s because the growth in the number of appliances has to some extent been balanced by the fact that appliances and lighting have been more energyefficient. Implemented policies and measures With a view to reducing both the direct and the indirect emissions of CO2 from the domestic sector, a wide range of initiatives have been launched. The object is to promote:
The initiatives to promote electricity savings include labelling schemes. The EU's obligatory energy labelling scheme for electric appliances, which has gradually been expanded to include new groups of appliances, has been given high priority, and a number of initiatives have been carried out to spread knowledge of the scheme. In addition, work is going on with a voluntary labelling scheme for TVs, videos and office equipment with respect to standby consumption. The labelling schemes have had a considerable impact. Firstly, they work in themselves and, secondly, they have formed the basis for a number of campaigns etc. The Electricity Saving Trust was established in 1997. Among the Trust's schemes is a grant scheme designed to encourage conversion from electric heating to district heating or natural gas in the domestic sector and the public sector. In addition, the Trust contributes to development, marketing and use of electricitysaving appliances. Table 4.10
The grid, district heating and natural gas distribution companies are required to promote energy savings within their supply areas, and they are carrying out a number of campaigns, information activities, advisory work, etc. These activities are funded via the companies' tariffs. More general measures include regular increases in the CO2 and energy taxes up through the 1990s. The increases have mainly affected households, helping to reduce their energy consumption. As a consequence of the initiatives in the domestic sector, energy consumption for space heating is expected to fall slightly even though the number of m2 housing is rising. From 2001 to 2010, energy consumption for this purpose is expected to fall by 2%. Relatively speaking, oil consumption will be reduced most, namely by 20%, while electric heat consumption will be reduced by 8%. On the other hand, consumption of district heat, natural gas and biofuels will increase by some per cent. CO2 emissions will thereby be reduced, particularly when district heat is produced with CHP or with CO2 friendly fuels. Electricity consumption for appliances is expected to increase slightly - by 3% - up towards 2012, compared with today's level, which is 30 PJ/year. Although efficiency improvements are expected in many appliances, electricity consumption for this purpose will not fall because households are acquiring more appliances. Additional policies and measures As follow-up on the climate strategy, new energy-saving initiatives are expected to be launched, including in the form of codes for products' energy efficiency. The actual implementation of the initiatives has not yet been decided. The extent to which costeffective energy savings etc. can be initiated will be assessed on an ongoing basis. The waste sector's contribution to greenhouse gas emissions consists only of methane from decomposition of organic waste at landfill sites. Methane, CH4 Previous years' action in the waste sector has been based on "Action Plan for Waste and Recycling 1993- 97", which includes objectives concerning handling of waste up to the year 2000. The plan does not relate directly to the waste sector's contribution to methane emissions (CH4), but includes a number of initiatives that are of relevance to waste products containing industrial gases (HFCs and SF6), besides an objective concerning stopping landfilling combustible waste. The previous government's waste plan,Waste 21, which covers the period 1998-2004, does not relate directly either to the waste sector's possibilities for contributing to solution of the problem of greenhouse gas emissions. The plan is aimed at stabilising the total quantities of waste in 2004, increasing recycling and reducing the environmental burden from the environmentally harmful substances in waste, including the industrial gases. With respect to waste incineration, the objective is to adjust incineration capacity to what is absolutely needed, to ensure best possible energy utilisation, maximum CO2 displacement and regional selfsufficiency. The plan thus contributes indirectly to reduction of greenhouse gas emissions. The objective in Waste 21 is for 64% of all waste to be recycled, 24% to be incinerated and not more than 12% deposited. That objective was already reached in the year 2000 according to the Danish Environmental Protection Agency's Waste Statistics 2000 (ISAG). Total waste in that year amounted to about 12.8 million tonnes. The present government has initiated the preparation of a replacement for Waste 21 in the form of a waste strategy for the period 2005-2008. The strategy is expected to go before the Folketing in May/June 2003. Implemented policies and measures The waste sector's contribution to reduction of Denmark's greenhouse gas emissions consist mainly in
Methane emissions from Danish landfill sites are calculated to have amounted to 64,000 tonnes gross in 1990, rising to a maximum gross emissions of 68,800 tonnes in 1996/1997, corresponding to 1.2 million tonnes CO2 equivalents. As a consequence of the ban on landfilling combustible waste from 1 January 1997, methane emissions from Danish landfill sites will fall in the years ahead. Calculations show that in 2012 the methane emissions will be 47,600 tonnes, corresponding to a 30% reduction in relation to the maximum methane emissions in 1996/1997. According to the Danish Energy Authority's inventory "Biogas, Production, Forecast and Target Figures", there were in all 25 biogas plants in Denmark in the autumn of 2002. 10,000 tonnes of methane are recovered yearly from these plants. For comparison, only 1,700 tonnes of methane were recovered in 1990. As a consequence of the new landfilling strategy, only a few biogas plants are expected to be established in the period up to 2012. The maximum quantity of methane recovered is expected to be about 12,000 tonnes in 2002/2003. Thereafter, the quantity of methane recovered is expected to remain at the same level for some years and then to fall steadily over a long period of years. On the basis of the abovementioned net emissions of methane (methane produced less methane recovered) from Danish landfill sites are calculated to be 62,400 tonnes in 1990, rising to 65,500 tonnes in 1994, and then falling steadily to 38,500 tonnes in 2012. The average annual net methane emissions in 2008-2012 correspond to about 0.9 million tonnes CO2 equivalents. The total quantity of waste incinerated rose from 2,216,000 tonnes in 1994 to 3,221,000 tonnes in 2001, i.e. an approximately 45% increase. The energy produced from the incineration plants is included as part of the renewable energy production in the Danish energy statistics. The international greenhouse gas inventories include greenhouse gases from incineration of the waste's content of oil-based products, such as plastics. In accordance with the objectives of Energy 21 and Waste 21, efforts are being made to design the incineration plants for maximum energy utilisation. Besides the direct effect of waste handling on greenhouse gas emissions, the emissions are also affected indirectly through recycling of paper, cardboard, etc. which means less energy consumption and thus less CO2 emissions during production of new products. With increased recycling of organic waste in biogas plants and use of the methane in biogas engines it is important for the methane emissions from the engines to be reduced either via development of technology or by flaring the flue gas. The implementation of the government's waste plans and achievement of the objectives set in this area have necessitated the use of a wide range of policies and measures. An amendment of the Statutory order on Waste in 1996 introduced a municipal obligation to refer combustible waste for incineration (corresponding to a ban on landfilling combustible waste). As a result of this instrument, large quantities of combustible waste that used to go to landfill sites are now either recycled or used as fuel in Denmark's incineration plants. Besides the traditional regulation via legislation, statutory orders, and circulars, the waste sector is regulated by means of a range of policies and measures, including taxes and charges, grant schemes and agreements. Since the introduction of the waste tax in 1993 the tax has been differentiated to reflect the prioritisation of the different forms of treatment. It thus costs most to deposit waste, less to incinerate it and nothing in tax to recycle it. The size of the tax thus provides an incentive to recycle as much of the waste produced as possible and to use non-recyclable, combustible waste as fuel in energy production instead of depositing it at a landfill site. Weight-based taxes (e.g. on various packaging, carrier bags and PVC film) encourage a reduction in packaging consumption and thus the quantities of waste. The weightbased tax is based on an index that reflects the environmental burden of the materials used. Besides the waste tax, which the local authorities collect to finance the public waste treatment, increasing use is being made of fees to finance, for example, return agreements for special waste fractions, including tyres and lead accumulators. The fees are used in this context to finance collection and recycling of the waste. Under the grant programme "Programme for Cleaner Products etc.", grants are made for projects that reduce the environmental burden in connection with development, production, sale and use of products or in connection with the handling of the waste that is generated during the product's entire life cycle. Grants can also be made for waste projects aimed at reducing the problems in connection with waste disposal. 4.3 Energy policies and measures in GreenlandUntil the publication of the Greenland Energy Plan 2010 in 1995, the all-important energy policy objectives in Greenland were security of supply and the energy policy guidelines from 1986, the main focus of which was hydropower. With Energy Plan 2010, the Home Rule presented a complete review of the energy sector and an action plan for its development for the first time and set up a more differentiated main energy policy objective of "establishing an energy supply that does not compromise security of supply and that ensures the least possible economic and environmental burden for society and the other energy players." Both before and since 1995, policies and measures have been adopted and implemented in the energy sector that have reduction of greenhouse gas emissions as one, although not in most cases the main, objective. Some of the most important measures are described below. Act on Energy Supply With adoption by the Landsting of the Act on Energy Supply in 1997, Greenland got for the first time legislation that deals with energy supply in a broad perspective, since it covers electricity, heat and fuel supply. At the same time, it is the first time that energy efficiency improvement and energy savings have been covered by legislation. This Act confirms Energy Plan 2010's main objective of promoting the most economic and environment friendly energy supply. It is stated in the Act that the energy supply shall be planned with a view to economising and saving in energy consumption, the highest possible level of security of energy supply, efficient improvements in the production and supply system and cleaner energy production. Use of hydropower for energy supply Since the 1970s the Home Rule has been interested in using hydropower for energy supply. Up through the 1970s and 1980s systematic studies of possible hydro power potentials were carried out. With the presentation of the energy policy guidelines in 1986, it was agreed that hydropower should be a bearing element of the future energy supply system. The first hydropower plants, taken into use in 1993, supplies Nuuk with electricity. Since it was commissioned, the plant has resulted in an annual saving of more than 20,000 m3 oil, which has resulted in a reduction in CO2 emissions of around 55,000 tonnes, or about 10% of the total CO2 emissions in Greenland. A hydropower plant to supply Tasiilaq is under construction. It will go into use in 2004. The expected oil saving with this hydropower plant is 1,300 m3, corresponding to 3,446 tonnes CO2 per year. A third hydropower plant is expected to be built within the next couple of years to supply Qaqortoq and Narsaq in South Greenland, with displacement of oil corresponding to 4,800 m3. Greenland also has a 10-year plan for further expansion of hydropower. Waste incineration Waste incineration plants have been built in three villages and in a number of small communities with waste disposal as the main objective. At all three plants in the villages, some of the surplus heat from the incineration process is used for district heating. A further three incineration plants are under construction in other villages. There, the heat will also be used for district heating. The existing waste incineration therefore to some extent replaces fuel oil and results in an unmeasured reduction of methane emissions that would occur if the waste were deposited at landfill sites. Sector Programme for Renovation with an Environment and Energy Improving Effect in Greenland 2000-2003 In 1999 the Home Rule and the Danish State entered into an agreement on renovation of buildings and supply plants. The agreement covered renovation projects with a positive environmental and energy effect. Projects carried out under the programme include renovation of electricity and heat production plants, including supply grids, revision of the building regulations, renovation of buildings, including the climate envelope, preparation of a new energy plan and behaviourregulating measures. All the initiatives are expected to help reduce energy consumption and, consequently, CO2 emissions.
5 Projections and the total effect of policies and measures5.1 Introduction and overall effect of policies and measuresAccording to the EU's burdenssharing agreement, Denmark must reduce greenhouse gas emissions by 21% in the period 2008-2012 in relation to the base year 1990/95 under the Kyoto Protocol. In connection with the agreement, Denmark took reservation in a declaration for the effects of a large import of electricity from Norway and Sweden in the base year 1990, which resulted in Denmark emitting 6.3 million tonnes CO2 less than would have been the case if the electricity had been produced in Denmark. The Danish position was, and is, that a fortuitous event such as a large electricity import in a single year should not mean that Denmark's reduction obligation in relation to the EU should be calculated on the basis of the random low emissions in 1990. In March 2002 Denmark had to accept a Council decision that binds Denmark legally to a reduction of 21% in relation to the emissions in the base year, which has not been adjusted for the electricity import. Denmark was, however, assured in a political declaration from the EU Council of Ministers and the European Commission that the assumptions relating to base year emissions will be taken into account in connection with fixing the permitted amount of emissions in 2006, measured in tonnes of CO2 equivalents. The government will therefore work to ensure that Denmark's reduction burden in 2008-2012 corresponds to 21% of the 1990 level adjusted for electricity import, corresponding to 5 million tonnes CO2 equivalents per year. The shortfall in respect of fulfilling Denmark's obligations with the existing policies and measures has been calculated partly for a situation in which account is taken of the electricity import in 1990 and partly for a situation in which account is not taken of this. The projections are based on a number of sector-specific projections of the domestic emissions for this period. These emissions depend on the scope of economic activity in all sectors of society, energy prices, technological development and the legislation regulating the various activities with respect to environment, energy efficiency, etc. The main assumptions include the Ministry of Finance's estimate concerning economic development1 and the IEA's expectations concerning future energy prices2. In addition, the projections are based on already adopted regulation of various sectors, including the environmental regulation of agriculture and the energy sector. According to the latest inventories of greenhouse gas emissions, Denmark's reduction obligation of 21% means that the emissions must be reduced from 69.5 million tonnes CO2 equivalents in the base year 1990/95 to 54.9 million in the period 2008- 2012. The latest projections from February 2003 cover the period 2001-2017 and are reproduced in Appendix B. However, the calculations for the period 2013 - 2017 must be described as somewhat less certain than the projections up to 2013, in part because of the uncertainty concerning the policies and measures and their expected effect increases with time. In addition, new projections have not been carried out for the agricultural sector after 2012. The projection is a "with measures" projection that includes initiatives that can be expected with reasonable certainty to be implemented without further political action in the form of legislation, political agreements or similar. The projection must therefore not be confused with the most probable development because it does not take account of new political initiatives that could be taken according to the government's climate strategy, February 2003, which was adopted by the Folketing on 13 March 2003. It should be noted that the latest historical inventory of greenhouse gas emissions covers the period 1990- 2001, for which reason the projection for 2001 in this report has been replaced by the historical inventory for 2001. Since this new inventory also includes an update of the 1990 figures as a consequence of new knowledge, the base year - and thus also the shortfall - has been changed slightly in relation to the inventory in the climate strategy. Denmark's expected annual emissions in the period 2008-2012 have been calculated to be 80.1 million tonnes CO2 equivalents. As will be seen from table 5.1, the size of the total greenhouse gas emissions depend greatly on CO2 emissions associated with electricity export, which is estimated to be 9.9 million tonnes CO2 equivalents per year in the period 2008-2012. Table 5.1.
5.2. Energy, including transport and the domestic sectorIn this section the projection of the emissions of CO2, CH4 and N2O from combustion of fuels and from gaseous emissions from fuels is described. The projection includes all fuel-consuming sectors, including the transport sector and industry. The projection is based on a projection of the development in energy consumption in the period 2002-2017. The emissions of CO2, CH4 and N2O have been calculated by multiplying the energy consumption by emission factors. The projection of energy consumption is based on the initiatives described in sections 4.2.1 - 4.2.3 and 4.2.5 being implemented and on no further initiatives being implemented. It should therefore be seen as a "with measures" projection. Figure 5.1 and table 5.2 show the development of total energy consumption (excl. fuels for non-energy purposes) with this assumption, broken down by sector.
Figure 5.1 Source: Danish Energy Authority In years with ample precipitation Denmark is a net importer of electricity produced at Norwegian and Swedish hydropower stations, while in years with scanty precipitation, it is a net exporter of electricity to Norway and Sweden. This has resulted in large fluctuations in the observed Danish gross energy consumption in the period 1990-2001. Table 5.2
Source: Danish Energy Authority
Figure 5.2 Energy consumption is expected to grow within most business sectors and transport in the next 15 years, but to fall slightly in the domestic sector. The energy sector's consumption has been calculated excluding fuels for production of electricity for export because this consumption figures separately, but the calculation includes flaring. Domestic electricity consumption is expected to grow, which is also reflected in the gross energy consumption in the energy sector up to 2013. Thereafter, the sector's energy consumption falls because a number of primary coalfired stations are expected to be replaced by new, more efficient CHP plants, about half of which are expected to use natural gas as fuel. As will be seen, the big increase in total energy consumption in the first part of the projection period is due to a big increase in electricity exports. This increase is expected partly because the price of electricity on the Nordic electricity market is expected to rise and partly because the existing national CO2 Quota Act for the electricity sector only has an effect up to and including 2003. With that, it will be more attractive for the electricity sector to export electricity. Figure 5.2 shows the development of total energy consumption, broken down by fuels, which determine the size of CO2 emissions because the fuels have very different emission factors. The increase in the quantity of renewable energy up to the year 2004 is due primarily to expansion of wind turbines, while the increase in oil consumption can be attributed mainly to growth in the transport sector. With the new power stations, natural gas consumption increases from 2014 at the expense of coal consumption. This change means a reduction in CO2 emissions because natural gas has far lower emission factors than coal. As will be seen later, with the expected development of energy consumption the CO2 emissions from Danish territory will exceed the Kyoto objective for 2008-2012. An EU Directive on trading with CO2 emissions from electricity and heat production, together with fuel consumption in certain sectors of industry, is expected to play a vital role in costeffective achievement of Denmark's Kyoto target. Table 5.3 shows the resulting emissions of CO2, CH4 and N2O from the energy sector in the "with measures" projection. The emissions of CH4 and N2O calculated as 1000 tonnes are CO2 equivalents. Appendix B contains detailed tables showing the results of the projections. Table 5.3
Source: 1990-2001: National Emission Report (NIR), National Environmental Research Institute, April 2003, 2002-2017: Environmental Project No. 764, Danish Environmental Protection Agency, February 2003 and Danish Energy Agency 5.3. Business sectorBesides the greenhouse gas emissions mentioned in section 5.2, industrial processes include a number of activities that emit greenhouse gases. This section covers emissions connected with production of cement, chalk and bricks, together with emissions of the industrial gases HFCs, PFCs and SF6. The projection of the emissions is based on implemented and adopted policies and measures, described in chapter 4, including a statutory order on phasing out certain industrial gases. This statutory order will result in a reduction in greenhouse gas emissions of, on average, 1.1 million CO2 equivalents per year in the period 2008-2012. It is covered by a ban on the use of HFC as a coolant in the retail trade and stationary A/C systems from 1 January 2007, except for refilling of existing systems, and as a foaming agent in PUR foam from 1 January 2006. 5.4 Agriculture16% of Denmark's greenhouse gas emissions in 2001 consists of methane and nitrous oxide, which are primarily emitted by agriculture. The methane and nitrous oxide emissions are not taxed and are only regulated indirectly via the regulation of the effect on the aquatic environment of nitrogen losses from agriculture, e.g. in the Action Plan for the Aquatic Environment II. Further possibilities for reduction of the methane and nitrous oxide emissions in the agricultural sector have not been sufficiently identified at present. More knowledge is needed on both technical possibilities for reduction and the associated costs. Owing to the EU's milk quotas and the increasing productivity within dairy farming, the cattle population is expected to fall by 1.8% per year to 524,000 dairy cows in 2010. In pig farming, on the other hand, production is expected to rise by 1.5 % per year. This will result in increased production of fatteners to just over 26 million in 2010. In total, the fall in cattle population and the rise in pig population are expected to result in a small increase in the total quantity of manure. Total agricultural land is expected to fall by 0.3% per year. In addition, the planned afforestation area has been deducted. It is also assumed that agricultural land used for organic farming will reach 220,000 ha in 2010. The area with set-aside crops according to the EU's subsidy schemes is estimated to be 7% of the total agricultural area in the entire projection period. 5.4.1 MethaneIncreasing productivity of individual cows means a rise in the emissions coefficient for methane from dairy cows from 102 kg methane/cow/year in 1990 to 117 kg methane/cow/year in 2010. However, this is more than balanced by the fall in the population of dairy cows, and the result is a fall in methane emissions (table 5.6). 5.4.2 Nitrous oxideThe fall in nitrous gas emissions shown in table 5.7 can be attributed particularly to reduced use of nitrogen fertilisers and a fall in nitrogen leaching and ammonia evaporation, which are effects of the action plans for the aquatic environment area. It is assumed that the aquatic environment action plans (Action Plans for the Aquatic Environment I and II) will be fully implemented in 2003. Table 5.4
5.5 ForestryThe projections for CO2 sequestration in forests are based on an assumption that the present subsidy structure and financing are maintained until the end of 2012. So far, financing has been made available until the end of 2003, and political commitment for public financing and/or access to alternative sources of financing for private afforestation may be available even beyond 2003. Table 5.8 shows the expected rate of afforestation in selected years up to 2020. Indeed, the rate of private afforestation will depend on the economic conditions in the agricultural sector, and, as the marginal agricultural localities are planted over time, a saturation point may be reached where the existing subsidies no longer provide an incentive for further afforestation. 5.6 WasteThe objective of the waste plan - Waste 21 - is to reduce the proportion of waste going to landfill sites from 2.1 million tonnes (16%) in 1997 to 1.5 million tonnes (12%) in 2004. As mentioned earlier, this target was already achieved in 2000. The net methane emissions (produced methane less recovered methane) from Danish landfill sites is calculated to be 62,400 tonnes in 1990, rising to 65,500 tonnes in 1994 and then steadily falling to 38,900 tonnes in 2012. The average annual net methane emissions from landfill sites in 2008-2012 correspond to about 0.9 million tonnes CO2 equivalents. There are no emissions of methane from wastewater in Denmark because wastewater is treated with aerobic processes. Table 5.8 Table 5.9
5.7 Total emissions5.7.1 Total carbon dioxide (CO2) emissionsTable 5.9 shows the expected development of CO2 emissions, while Appendix B gives a more detailed projection. The biggest source of CO2 emissions in Denmark is combustion of fossil fuels, including electricity and heat production and transport. The transport sector has had the biggest increase in CO2 emissions since 1990, and the emissions are expected to continue rising for the whole of the projection period. The CO2 emissions from the transport sector were 10,404 Gg in 1990 and rose to 12,077 Gg in 2001, while in the period 2008-2012 it has been calculated that the average annual CO2 emissions will be 13,727 Gg. The emissions from energy production, including conversion and distribution, fluctuated in the period 1990- 2001 due to greatly varying electricity export/import. The CO2 emissions from energy production were 26,202 Gg in 1990 and 26,375 Gg in 2001, while for the period 2008-2012 it has been calculated that the average annual CO2 emissions will be 35,405 Gg, of which 9,900 Gg can be attributed to electricity production for export. Table 5.10
5.7.2 Methane,CH4Most of the methane emissions come from farm animals' digestive systems. The reduced emissions from 1990 to 2001 and continued reduction in the projection period can be attributed mainly to a smaller cattle population. The second-largest source of methane emissions are landfill sites, where emissions also decreased from 1990 to 2001. However, the energy sector's methane emissions increased considerably in the same period due to increased use of gas engines. Total methane emissions were 5,672 Gg CO2 equivalents in 1990 and 5,606 CO2 equivalents in 2001, while in the period 2008-2012, is has been calculated that the average annual emissions will be 4,979 CO2 equivalents. Table 5.11
5.7.3 Nitrous oxide,N2OAgriculture is by far the biggest source of emissions of nitrous oxide because this can form in soil through bacterial conversion of nitrogen in fertiliser and manure spread on fields. The main reason for the reduction in total nitrous oxide emissions from 10,843 Gg CO2 equivalents in 1990 to 8,749 Gg CO2 equivalents in 2001 is a combination of the Action Plans for the Aquatic Environment I and II and the Action Plan for Sustainable Agriculture. In the period 2008-2012 calculations indicate average annual emissions of 8,738 CO2 equivalents. The contribution from the transport sector and the energy sector to nitrous oxide emissions is expected to rise, while the contribution from agriculture is expected to fall slightly in relation to 2001. 5.7.4 Industrial gases HFCs, PFCs andSF6In accordance with the possibilities offered in the Kyoto Protocol, Denmark has chosen 1995 as the base year for emissions of the industrial gases HFCs, PFCs and SF6. The total emissions of these gases were 344 Gg CO2 equivalents in 1995 but double that - 793 Gg CO2 equivalents - in 2000. In 2001 the emissions fell to 700 CO2 equivalents. Table 5.12
Source: Nukissiorfiit. The main reasons for this were the introduction of a tax and legislation on phasing out import, production, and use of these gases. For the period 2008-2012 calculations indicate total average annual industrial gas emissions of 706 CO2 equivalents. Thereafter, a considerable reduction is expected in HFCs, which are the largest contributor to industrial gas emissions, and overall this will result in a considerable reduction of industrial gas emissions after the first commitment period. 5.8 Greenland and the Faroe IslandsWith respect to the expectations concerning future greenhouse gas emissions in Greenland, the projections cover only electricity and district heat production. The projections for CO2 emissions from electricity and district heat production are based on a projected increase in energy consumption of 1% up to 2005 and then stagnation. The projections are also based on the fact that a hydropower station is under construction and expected to go into operation in 2004 and that a further hydropower station is planned, which will go into operation in 2006. There are not at the present time any estimates of future greenhouse gas emissions on the Faroe Islands. 5.9 Methods used in the projectionsThe projection of energy consumption in the business sector and the public service sector is based on an ADAM/EMMA projection, while the domestic sector is projected on the basis of the bottom-up principle. EMMA is a macro model that describes the final energy consumption broken down into a number of sectors and seven types of energy. It is based on historical experience with the behaviour of businesses and households and is documented in satellite models for ADAM, NERI Technical Report No. 148, DMU 1995. In EMMA, energy consumption in the business sector is determined by three factors: production, energy prices/taxes and energy efficiencies/ trends. Increased production will increase the demand for energy input, whereas increased energy prices and taxes will pull in the direction of a more limited demand for the fuels. Improved energy efficiency will mean that production can be maintained using less energy, and in EMMA this results in reduced energy consumption. The projection of production is based on the ADAM projection in the Economic Report, January 2002, covering the period 2000-2010. For the period 2011-2017 figures from the Financial Report 2001 have been used. The domestic sector's energy consumption has been determined using the bottom-up models: the Electricity model for households and the Heating model for households. The projection is based on, among other things, expectations concerning growth in the housing stock and expectations concerning the development in the number of electric appliances. The projection of electricity and heat production is based on the Danish Energy Authority's RAMSES model, using as the basis the demand for electricity and district heat according to the projection of the consumption sectors. In the projection, electricity and heat production is divided between existing and possible new production plants on the basis of technical and economic parameters. Industrial and local mini-CHP production is not projected in the RAMSES model so a separate (bottomup) projection has been made of this production. Table 5.15 The projection of road transport, rail transport, domestic ferries and freighters, together with domestic air transport is documented in the report "The transport sector's energy consumption and emissions", Danish Road Directorate, 2002. The projection is based on, among other things, the same economic assumptions as the EMMA projection above. The armed forces' consumption of transport energy is kept at a level corresponding to the average for 1998-2001. International shipping and border trade with diesel are kept at the 2001 level. Tables 5.14, 5.15 and 5.16 show a number of key figures and key assumptions for the projection. Additional information on the methods used in the projections is available in Environmantal Project No 764, published by the Danish Environmental Protection Agency in February 2003. Table 5.16 Table 5.17
6 Vulnerability assessment, climate change impacts and adaption measures6.1 Climate in the futureFuture climate change as a consequence of man-made impacts through increased greenhouse effect, depletion of the ozone layer and aerosol emissions are evaluated by means of climate models. Climate models, which are based on the laws of physics and ascertained relationships, are mathematical descriptions of the components of the climate system: atmosphere, ice, ocean, and snow, land surfaces and the biosphere. The calculations are performed in a large computer system and the models are becoming increasingly complex. 6.2 Climate trend in Denmark6.2.1 The latest developmentsDenmark is situated on the west side of the European continent, between the mainland and the Scandinavian peninsular in a marine area and therefore has a coastal climate. DMI's statistics1 show that the average mean temperature in the 1990s was slightly more than 8°C after having risen just under 1°C since 1870. The mean temperature is almost 16°C in the summer quarter and around 0.5°C in the winter quarter. Average annual precipitation (measured values before precipitation adaptation) in the 1990s was about 735 mm and has thus risen by almost 100 mm since 1870. There are, however, significant regional differences. West and Southern Jutland have most precipitation (over 900 mm) and the Eastern islands less (slightly more than 500 mm). The water level in Danish waters has generally risen in the last 100 years, but after adjustment for land movements, there has been no general rise in water level in Danish waters. However, since Denmark tilts, the water level in the southern part of the country is rising by about 1 mm per year. Unfortunately, the region in question has many low-lying, vulnerable areas. 6.2.2 Projected climate changes in DenmarkFor several reasons, the basis for evaluating the impacts of the manmade increase in the greenhouse effect is uncertain. Serious problems are that the magnitude of future greenhouse gas emissions is uncertain and that the climate models are encumbered with uncertainty. DMI/Denmark's Climate Center (in cooperation with, inter al., Max Planck Institut für Meteorologie in Hamburg) has carried out global and regional calculations for several scenarios for future emissions of greenhouse gases and aerosols - namely, IPCC's IS92a-Business-asUsual scenario and the new A2 and B2 scenarios from IPCC's special report - SRES-2000 - on emissions scenarios2. Calculations with global and regional climate models show the following trend for the climate in Denmark in 2100 compared with 1990:
There would be a combined effect on the run-off, i.e. the water running in watercourses. For Denmark, there would be an increase of the order of 10% in the period December to April. A generally larger run-off of storm water in the Baltic region could make the surface water in the inner Danish waters less saline. This could affect fish stocks. The calculations carried out do not directly provide scenarios for future changes in the water level around Denmark, but previous studies4 show that the rises in water level around Denmark would be slightly smaller than the average global rises because of vertical land movements. For example, it is estimated that an average global rise in water level of 0.5 m would lead to a rise of about 0.4 m around Denmark. These figures do not account for the regional impact on water level of changed ocean currents, flow, temperature, and wind conditions. The wind effect alone gives a rise of 3-5 cm5. IPCC estimates that the global water level would rise 0.1-0.9 m in the period up to 2100 in the SRES scenarios. In Danish impact and vulnerability studies, rises in water level of 0.25- 0.50 m are usually used. 6.2.3 Impacts and Denmark's possibilities for adaptationEarlier evaluations The impacts of possible climate changes in Denmark have been evaluated several times since 1988 and most recently with various aspects in the report: "Climate Change Research - Danish Contributions" edited by A.M.K. Jørgensen, J. Fenger and K. Halsnæs in a cooperative project between DMI, NERI and Risø and published by DMI in 2001, and have been treated in greater detail in the report "Danish adaptation to a changed climate" (J. Fenger and P. Frich), published by NERI in 2002. The general conclusion has been that the direct impacts in moderate climate scenarios would be modest and could be countered by suitable ongoing adaptation. Danish studies of - and preparations for - impacts from climate changes have been very limited in their scope, and no action plans yet exist. However, the Danish Nature Council recommended in a report from 2000 (Vismandsrapport 2000) that preparedness be built up against the consequences of climate change for nature. It is suggested that the preparedness be based on technical reports and that relevant monitoring of nature follow it. There have not as yet been any evaluations of secondary impacts for Denmark in the form of changed tourist destinations, environmental refugees, etc. or any evaluations of impacts from changed conditions in other countries on a little, open economy like Denmark. For an exportoriented industry like Danish agriculture, such secondary impacts could easily be more important than the primary impacts. Water resources The quantity of water resources is affected by both the availability of water from nature and water consumption. With the prospect of summers that may be both hotter and drier, an increased demand for water for several purposes can be expected:
There is a fundamental difference between free groundwater reservoirs, where the formation of groundwater depends on the net precipitation, and artesian reservoirs, where the formation of groundwater depends mainly on pressure differences between upper and lower reservoirs. Moraine areas are generally less vulnerable to climate change than areas with sandy soil. Besides this, however, a permanent climate change can be expected to affect land use (other crops, longer growing season) and, through this, the size of the evapotranspiration. Similarly, a change in the pattern of precipitation in the form of increased intensity could affect the run-off pattern and thus also the formation of groundwater. Just as important as the quantity of groundwater is its quality, and here, the climate plays a role, albeit an indirect one. In Denmark, almost all fresh water is produced in potable water quality and from groundwater. Salt (NaC1) in the water is normally due to deposits in the subsoil. Only in a few areas does penetration of seawater play an important role such as small islands, e.g. Langeland and Samsø, and near low-lying coasts, e.g. along Køge Bay. With a rising sea level, salt penetration would increase and can be expected to reduce water recovery in slightly more places than is the case today. Agriculture The combined impacts are expected to benefit Danish agricultural productivity. Changes in cultivation practice can be implemented at short notice, and production is expected to increase with rising temperature and CO2 concentration. There is at present a trend towards less cattle production and more pig and grain production. The projected climate changes could reinforce this trend because market constraints in the dairy sector would limit production and more land and grain would be available for pig production at competitive prices. However, higher temperatures would increase the risk of pests and plant diseases resulting in an increased demand of pesticides. At the same time, increased production would require more fertilisers, which, together with more precipitation and higher winter temperatures, would increase the risk of nitrate leaching. Here, it might be necessary to change the environmental legislation to ensure a costeffective agricultural sector and protect water resources in a changed future climate. Forestry Danish forestry is characterised by a long duration of production determined by the rotation age of the trees, which is between 50 and 180 years. Long-term planning based on the most suitable species and genotypes in an optimal forest structure is therefore necessary. Danish field and greenhouse studies have indicated that the projected climate change would promote tree growth, particularly for species with natural distribution having its northern limit in Southern Scandinavia. The only tree species expected to show decline is Norway Spruce, which has its natural distribution southwest of Denmark, but which has become the most common tree species in Denmark through planting. After the wind fall in December 1999 new planting of other species has become more widespread. Forests are important carbon sinks, and reforestation, deforestation, and afforestation figure in the national CO2 inventories. The planned doubling of forest land in Denmark during the next 100 years could sequester around 5% of the national emissions. Natural ecosystems Denmark is centrally situated in a natural vegetation area with temperate deciduous forests, and this will not change significantly. However, many species of fauna and flora have the limit of their dispersal in or around Denmark, and a northward shift could therefore be expected. Not all alien species are equally welcome, particularly in agriculture. The Colorado beetle has its northern limit just south of Denmark. The progress of the Iberian forest snail in recent years may be connected with a generally milder winter climate. The spread of new species is made diffinational cult by the fact that the landscape is very fragmented. This may mean a reduction in species diversity for a time but can be remedied by Denmark's intensive nature preservation and management of nature. Freshwater ecosystems are sensitive to the quantity of water and can be burdened by reduced precipitation in the summertime. The effect may be intensified if increased leaching of nutrients occurs. Coastal protection The Danish coastline consists of raised beaches and wide foreshores in the northern part of the country and an archipelago to the south. The coastline is relatively long, about 7,400 km for an area of 42,000 km2. 80% of a population of 5.33 million (1.1.2000) live in urban areas connected to the coast. The vulnerable areas are particularly raised seabed, marshlands, and reclaimed land, where 60-70,000 properties are situated. Around 1,100 km of the coastline are protected by dikes and 700 km by other permanent installations. Increasing use is being made of soft solutions - particularly beach feeding. As yet, direct planning for rising water levels beyond the present secular rise is extremely modest and purely qualitative. However, some thought has been given to the possible impact on coastal ecosystems, particularly salt marsh and dune areas. Here, the pattern of action will depend on the attitude to - and weighing up of - economic, sociological and biological interests and possibilities. The general strategy seems to be in the direction of preservation of a natural coastline - at the cost of agricultural land if necessary6. Infrastructure In connection with the construction of coastal infrastructure, including bridges, harbours, sewerage installations, etc. the general attitude has been "wait and see". Economic evaluations have been unofficial or lacking altogether. However, in connection with the planning of the new metropolitan district "Ørestad" on the partially reclaimed land on the island of Amager near Copenhagen, a rise in water level of around 0.5 m was taken into account for the stairs leading down to Metro stations. Fisheries Higher temperatures and lower salinity in Danish waters would affect the survival, growth, and reproduction of the present fish population. It would also result in a longer growth season for plankton and thus favour species that directly live from plankton. This could include sardines7. Energy consumption Denmark has a reasonably cool climate now and no tradition for air conditioning (although many new cars are now fitted with an airconditioning system). Less need for heating would therefore presumably mean lower energy consumption. Health and well-being In the next 100 years the projected climate change would hardly give Denmark a climate that differs significantly from today's climate in, for example, Northern France. Direct health impacts in the form of a higher risk of heat stroke or a reduced risk of colds can therefore not be expected. On the other hand, a number of indirect impacts can be predicted. A considerably larger amount of pollen and a several weeks' earlier start to the pollen season have already been observed. This could be the reason for the increase in allergy cases. In addition, vector-borne diseases could occur with invasion by, for example, malarial mosquitoes. Infection via refugees (possibly environmental refugees) and immigrants would increase the risk not only of "southern" diseases, but also of diseases that are at present under control in Denmark - e.g. tuberculosis. A warmer climate could also increase the risk of photochemical air pollution, which, in Denmark, is mainly due to long transport from Central Europe and elsewhere. Greenhouse gas emissions A changed climate could in many cases mean changes in greenhouse gas emissions and thus a feedback effect on the climate system. Possible sources affected, besides energy production and forestry, are different forms of agricultural activities, including livestock (methane) and use of manure (nitrous oxide). The consequences of going over to organic farming have been discussed, although without any clear conclusions. 6.3 Climate changes in GreenlandGreenland has an arctic climate. 82% of the land is covered by the up to 3km-thick ice cap, while the icefree land areas are limited to a coastal strip up to some hundred kilometres wide. However, furthest south, the climate is sub-Arctic with a mean temperature of more than 10°C in the warmest month, while the climate in the rest of Greenland can be divided into a low-Arctic zone and a high Arctic zone. The low-Arctic zone, which extends northward to Melville Bay on the west coast and to Scoresbysund on the east coast, is characterised by relatively mild winters with a lot of snow and periods of thaw and summers with a mean temperature of 5-10°C in the warmest month and frequent rain. This description applies particularly to the maritime coastal zone, while, inland, Southwest Greenland has a winter climate that is more like high-Arctic. The high-Arctic region, which covers the entire northern and northeastern part of Greenland, has a continental climate with very cold winters (more than 50 degrees of frost occur in North Greenland), in which the temperature rarely rises above zero from September to May, and in which winter precipitation is limited. Parts of North Greenland have a desertlike climate with only about 25 mm precipitation per year, or about 1% of the precipitation at the southern point of Greenland. The continental climate in high-Arctic Greenland is due to field ice, which often constitutes a several-hundredkilometre wide belt of tightly packed polar ice that drifts down along the east coast and so to speak "extends" the land out to sea. The climate in highArctic Greenland is therefore greatly influenced by precisely the amount of field ice. Calculations with global climate models8 show the following general trend for the climate in Greenland in 2100 in relation to 1990:
Almost the entire population of Greenland live in towns and villages in the low-Arctic part of the country, with most living in Southwest Greenland, which has the mildest climate, and where the main industry is fisheries. Only in the southernmost part of the high-Arctic region, in Thule towards the northwest and in Scoresbysund on the east coast, are there small communities that live to some extent from hunting mammals and birds. A description is given in the following two sections of what could or would happen on land and in the marine environment as a consequence of the expected climate changes. The description is based exclusively on general evaluations9 with the present extremely limited knowledge concerning factors determining the welfare of the species and ecosystems in question10. 6.3.1 Impacts and adaptations in terrestrial ecosystemsThe very big differences between the climate in the low-Arctic and high Arctic parts of Greenland are reflected in marked differences in the natural conditions in the two parts. Low Arctic Southeast and West Greenland are characterised by luxuriant vegetation with bushes and often thick plant cover. In winter the snow often lies deep and soft from November to some time in May. Unlike this, in Northeast and North Greenland, the plant cover is usually only a few centimetres high, and increasingly large areas are entirely without vegetation as one moves northward. This is because of the poor snow cover, with many areas blown free of snow for most of the winter, while the rest is covered by often tightly packed snow that does not disappear until the end of June or the beginning of July. The Arctic fauna and flora, which, compared with the situation in more southern climate zones, are poor in species, are adapted to the extreme climatic conditions. Some plants, invertebrates, and mammals depend on stable snow cover to protect them from the cold. However, many other species are dependent on the snow disappearing early - or being blown away altogether in winter. The distribution, duration, and thickness of the snow cover are therefore just as important factors as the temperature in the general conditions of life for many plants and animals in Greenland. The importance of the snow cover As a consequence of earlier snow melting in low-Arctic Greenland, higher summer temperatures and more summer precipitation, a long growth season can be expected and thus a more extensive and vigorous plant cover. Immigration of species from the south can be envisaged, but would be impeded by barriers in the form of the waters and competition from already established species. Conversely, species with a more northerly dispersal could disappear from southern areas. In high-Arctic Greenland, more ample precipitation in both summer and winter, together with slightly higher summer temperatures, would presumably mean increased growth and more extensive plant cover, and it can be envisaged that large parts of this zone would change character in the direction of low-Arctic conditions. However, the increased snow cover would delay melting, which would impede plant growth and delay plant reproduction or make it completely impossible. There would be a risk of more northerly species, such as sabine ranunculus, disappearing altogether. The increased UV-B radiation as a consequence of the depletion of the ozone layer, which is expected to continue for a couple of decades, would presumably cause problems in Arctic plants that are adapted to low UV-B radiation. The extent to which the plants would be able to adapt to the greater radiation is not known. The carbon balance and the permafrost Increased microbial activity and thicker active strata (the part of the earth that dries up on top of the permafrost) would also release more greenhouse gases, but in the case of carbon dioxide, this would be counteracted by a bigger uptake in the plants as a result of the increased growth. Owing to Greenland's very hilly landscape, there are not the very large layers of peat that are so widespread in parts of Siberia and Canada. For this reason, Greenland's contribution to the feared release of enormous quantities of carbon dioxide from such peat layers would presumably be modest. Mammals A great deal of Greenland's fauna would presumably also benefit from a milder climate and consequently more luxurious and widespread plant growth, although there are important exceptions. Many of the species in high-Arctic Greenland are dependent on the low-precipitation continental climate. This applies, for example, to the musk ox, where thicker snow cover and more frequent periods of thaw in winter (with the formation of ice crusts in the snow) could make it difficult for the animals to forage. Examples of this are already known with the present climatic conditions, and reindeer died out for the same reason in the whole of high-Arctic Greenland during a snowy period more than 100 years ago. The artificially established population of musk oxen in Southwest Greenland are hardly likely to suffer similar problems. On the contrary, both reindeer and musk oxen might thrive even better in the continental low-Arctic region. Birds Another "risk group" is the high Arctic waders, which are the dominant bird group in Greenland. Nine out of ten of Greenland's 11 species of wader are only found in - or have their main dispersal in the high-Arctic part. They are totally dependent on the sparse vegetation. Later melting of snow would also impede their reproduction since they are entirely dependent on early snow melting both in order to procure sufficient food, mainly in the form of early active arthropods and in order to be able to lay eggs on such large snowfree areas that the foxes cannot find all the nests. On top of this there is the prospect of the large wading areas that these birds make outside the breeding time in temperate and tropical climate zones being permanently flooded as a consequence of the expected rise in sea level. Immigration of new animal species Many insects and other arthropods could spread northwards, and new species, particularly of mobile insects and birds, could immigrate from the south, but they would undoubtedly come from regions where they are already common and would thus from a global point of view be unable to replace any loss of highArctic species, which would be definitive. Humans Seen from the point of view of local society, the changes mentioned in the terrestrial ecosystems would be of limited practical importance and perhaps even an advantage in the form of more plant growth, more reindeer and musk oxen and perhaps better possibilities for farming in South Greenland. The increased thawing of the permafrost could bring problems in areas where houses and other structures are founded in the permafrost, but since the vast majority of structures in Greenland stand on solid rock, the problem would only be a local one. Increased melting of the ice cap would provide more water - for hydropower for example - but this resource is not generally a constraint today. The cost of heating in winter would be reduced and there would be generally fewer problems in connection with hard frost. The possible loss of biodiversity, for example in the form of bird species in the high Arctic, would mean a loss of experiential quality, not only there but also in the birds' resting and wintering grounds. There would thus be a risk of most of the high-Arctic zone disappearing together with the special fauna and flora that are adapted to precisely this zone. Most of the continental high-Arctic areas are in North and North-east Greenland and on the northern Canadian islands. 6.3.2 Impacts and adaptations in marine ecosystemsIn North-east Greenland the expected climate change would result in the thickness of the ice halving in the fjords and a doubling of the icefree period. As a result, about 60% more light would penetrate down in the water column, which would stimulate the production of both plankton algae and bottom-living algae. However, the increased precipitation (snow) would impair the light conditions in the ice in early spring and probably have an adverse effect on the production of sea-ice algae and the animals that benefit from the early production. All in all, however, production would increase. Algae, water copepods, mussels, and walruses An increased fresh water supply as a consequence of increased precipitation and melting of the ice cap in the inner parts of the fjords would increase the water exchange in the fjords and bring more nutritious water in from the open sea and thus contribute still further to increased primary production. The increased production would have a powerful effect in the top levels of the food chain. Today, water copepods (crustaceans that live on algae) are limited by food, and stimulation of plankton production would immediately mean increased grazing and growth of copepods. Sedimentation of the copepods' faeces would therefore increase, thereby increasing the quantity of food for bottom-living animals. This would, for example, increase growth in mussels, which are today very limited by food. The increased mussel growth would benefit walruses. Rising winter temperatures would mean that the ice did not reach the same thickness as today and would therefore break up more easily in spring and that the walruses could seek food on the mussel banks for longer periods. Problems for polar bears The polar bear, on the other hand, is facing an uncertain future in East Greenland. If the ice disappeared it would reduce the bears' hunting grounds and they would probably follow the ice northwards. Seals, which are attached to the ice, would presumably become concentrated in smaller areas with ice and would therefore be more easily accessible to the bears, but in the longer term, the number of bears would decrease. In addition, the polar bear is not good at hunting seals in water. The ice conditions on the west coast of Greenland would probably not change as much as on the east coast, and the polar bears off the west coast would therefore be less affected by the climatic changes than those off the east coast. Fish Rising surface temperatures would also have a major effect on the composition of fish in the highArctic zone. In the case of rock trout, reproduction ceases when the temperature rises above 5°C because the enzymes in the egg sacs denature when the temperature is just a little over 5°C. As a result, the eggs rot in the body and the fish dies. At the same time, a number of Arctic fish species would be more exposed to parasites and bacterial and fungal attack, and their immune defence system would be reduced with rising temperatures. For many of Greenland's fish species, the seas off Greenland limit their dispersal, for example, cod, Norway haddock, striped catfish, halibut and herring, which have their northern limit there. Conversely, too high sea temperatures set a southern limit for the dispersal of Arctic species, such as polar cod, and Arctic roc. Therefore, relatively small variations in the temperature of the sea could result in considerable fluctuations in the dispersal of many fish species. The trend in cod fishing largely follows the average sea temperature. In the last 30 years, cod and a number of other boreal fish species have largely disappeared as a consequence of a generally colder climate in South and West Greenland. Today, more cold-adapted populations of prawn, crab, and halibut constitute the main commercial fishing resources in Greenland. A change in sea currents and a rise in temperature as a consequence of the climate changes would probably improve the conditions of life for cod and some other commercially exploited fish species in these areas. However, a larger cod population would have an adverse effect on the prawn population due to predation. It can therefore be envisaged that there would be a change in the fishing resources from dominance by prawns today to dominance by cod towards the end of this century. Crabs, copepods, and sea birds There are no crabs in areas with temperatures below 0.5ºC, which characterises large areas off East Greenland. The temperature rises in the future would perhaps mean that crabs would migrate into the area and thus distinctly change the composition of bottom-living animals. Another marked change that could happen is a change in currents, so that North Atlantic sea water containing a smaller species of copepod (Calanus finmarchicus) could penetrate areas that are today dominated by polar water with larger and longer-living species of copepod (C. Glacialis and C. hyperborus). If C. finmarchicus ousted the larger species it would have very serious consequences for little auks, which breed in their millions in the Thule area and around Scoresbysund, and which are specialised in foraging along the edges of ice with high concentrations of food animals. The little auk lives almost exclusively from the large species of copepod and could not get enough energy out of the little copepod. Polar guillemots, among other sea birds, would perhaps have more difficulty in West Greenland, but the populations there have already been reduced to some few per cent of the natural population by hunting, so the climate would undoubtedly be of secondary importance. Conversely, the Atlantic guillemot would be able to immigrate in large numbers in South-west Greenland, just as a number of other sea bird species would benefit from the increased marine production and the reduced ice cover. Whales Whales, which are associated with sea ice, such as the narwhale, the white whale, and the Greenland whale, would have reduced living areas in the winter months, while new areas would become available to them in the summer months. However, the reduced drift ice would mean reduced areas with concentrated food along the edges of the ice in the same way as for the little auk. In winter, the whales would get increased competition for food from other marine mammals. Other species of whale that use the Arctic and north boreal waters in summer would be able to use more northern areas. Our knowledge about the way the ecosystems function is constantly improving, but in the case of such large changes in such a short space of time, we as yet know too little to make precise predictions. One of the biggest uncertainties in connection with the marine environment in South Greenland is the extent to which the sea currents and thus sea temperatures follow changes in air temperature. The balance between the part of the seawater in Southwest Greenland that comes from the cold East Greenland Current and the part that comes from the warm North Atlantic drift (a branch of the Gulf Stream, which bends westward, south around Iceland), and the cold water masses in Baffin Bay and Davis Strait, thus totally determine the ecological conditions off Southwest Greenland, where most of Greenland's population live. Humans For Greenland society, a warmer climate would probably mean increased fishing in the form of more cod, Norway haddock and other species, but fewer prawns. The possibilities for hunting ring seals and polar bears would probably be reduced, while the occurrence of several other game animals would depend more on the pressure of hunting itself. Communication conditions would be much better because the period of open water would be longer, making it easier for boats to call at many towns and villages. There would be far less field ice, but on the other hand, a reduced possibility of using the ice to get from place to place. Retraction of glaciers and the ice cap, together with less "Arctic wilderness" could adversely affect the tourist industry, but the improved communication - including a longer summer season - could have a beneficial effect. 6.4 Climate changes on the Faroe IslandsCalculations with global climate models11 show the following general trend for the climate on the Faroe Islands in 2100 compared with 1990:
6.4.1 Impacts and adaptation in terrestrial and marine ecosystemsOnly minor changes in terrestrial ecosystems are expected. The isolation of the Faroe Islands in the Atlantic Ocean may have the consequence that climate-induced changes in plant and animal life will be unbalanced. Thus, the rate of possible species loss from terrestrial ecosystems may not be counterbalanced by a similar immigration rate, resulting in reduced species diversity. The greatest changes are expected at sea, although the uncertainty is also greatest here as long as the fate of the North Atlantic Current has not been clarified. Warmer deep water could result in a redistribution of pelagic and benthic communities. Impacts on plankton would be similar to those mentioned for Greenland. Fish species that settle in shallow waters in the early spring such as flatfish, lumpfish, and species with pelagic drifting eggs and larvae would have a high risk of UV-B induced damage. Effects on marine mammals and sea birds are expected mainly to concern spatial shifts in areas of food production and primary productivity (changes in upwelling sites), nesting and rearing sites, and increases in diseases and oceanic biotoxin production (from both temperature increase and current changes). The reappearance of cod seems highly dependent on what happens to sea currents. That there have been three to four times as many storms as normal in recent years has contributed to the disappearance of the cod by blowing the fry towards waters too cold for their survival. A reduction in water arriving from the south would worsen the present lack of the fry's favourite food.
7 Finacial resources and transfer of technology7.1 Danish development policyDenmark's vision for regional and global sustainable development is a world with economic development, social welfare, and greater protection of the environment. It includes a world market with free trade based on high environmental and social standards, and it includes respect for human rights, democratisation, transparency, and responsibility in administrations. Through both foreign policy and environment policy, Denmark will work actively to promote international action. Danish international assistance is still well above the UN objective of 0.7 per cent of GNI. Denmark attaches importance to ensuring coherence between development, environment, and trade policy. Denmark wants a strong global structure to promote all elements of global sustainable development, including a stronger structure for promotion of international environmental cooperation and environmental regulation. The effort to promote national sustainable development is closely linked to the global challenges for sustainable development - and vice versa. Growing trade and international capital flows, conflicts and refugee flows, together with the increasing pressure on natural resources, have made individual countries ever more dependent on the outside world. Denmark therefore has a great interest in contributing to sustainable development through national efforts and through the EU, the UN, the WTO, the OECD, and the international financial institutions, including the World Bank and the International Monetary Fund. The world is facing many regional and global challenges. Of the world's approximately 6 billion people, 2.8 billion live on less than 2 dollars a day and 1.2 billion live on less than 1 dollar a day. The challenge therefore consists primarily in eradicating poverty and creating better conditions of life for the poor people of the world. For example, one fifth of the world's people do not have access to clean water and sanitation, and this particularly affects women, children, indigenous peoples, and other particularly exposed population groups. The battle for scarce natural resources is in some cases the cause of violent conflicts, creating immense refugee problems, particularly in the developing countries. Analyses from the Intergovernmental Panel on Climate Change (IPCC) show that climate change is very probably already a reality, and it is in the developing countries that the greatest adverse effects of climate changes are expected. Biodiversity is under increasing pressure, and nature's resources are often used on an unsustainable basis. The use of dangerous chemicals is a growing problem, both for human health and for fauna and flora. There is often a close correlation between poverty and environmental problems. It is often the poorest people that are worst affected by the deterioration of the environment. At the same time, poverty limits the possibilities for sustainable utilisation of natural resources because limited resources are available for investment in protection of the environment. For example, poverty is contributing to soil exhaustion and desertification in Africa. Conversely, uncontrolled economic growth in developing countries and the slightly more developed countries in the East and South often leads to increased use of natural resources and burdens the environment. In its entire international work for global sustainable development, Denmark attaches importance to the need to integrate and balance the economic dimension (povertyoriented growth), the social dimension (promotion of such social sectors as education and health) and the environmental dimension (protection of the environment). Denmark will continue working for global sustainable development by
7.1.1 Development cooperationSince the change of government in Denmark in November 2001, the government has reviewed Denmark's development assistance and environmental assistance to developing countries with the objective of prioritising it, focusing it, and making it more effective. The agreed changes to the assistance on this basis mean, among other things, that more is required of the governments in the cooperation countries with regard to respect for human rights and democracy. Systematic and lasting violations of human rights and democratic rules of play will no longer be accepted. This has led to Denmark ending its assistance cooperation with Eritrea, Malawi, and Zimbabwe. This leaves Denmark with 15 programme cooperation countries - Bangladesh, Benin, Bhutan, Bolivia, Burkina Faso, Egypt, Ghana, Kenya, Mozambique, Nepal, Nicaragua,Tanzania, Uganda,Vietnam, and Zambia. The Danish development cooperation is financed mainly by the facility for assistance to developing countries (DKK 10.5 billion in 2002), the main purpose of which is to promote sustainable development through poverty-oriented growth. Equal participation by women and men in the development process, consideration for the environment and democratisation are of vital importance to combating poverty and are therefore integrated in all aspects of Denmark's assistance. In 1999 Denmark was awarded top marks in OECD's regular reviews of assistance to developing countries. The latest OECD review of Danish assistance took place in the spring of 2003, and the result of the review is pending. Thorough environmental analyses will play an essential role in the coming years' revision of the country strategies for Denmark's programme cooperation countries. Another important task will be to seek better integration of the objectives of international environmental agreements in the bilateral assistance cooperation. In the Appropriations Act for 2003 the government has chosen to prioritise a number of areas and to earmark further resources for them. The areas include good governance, assistance to refugees in local areas, environment, industrial development, women, and trade and development. Denmark seeks actively to get the many countries - including the EU countries - whose development assistance is below the UN objective of 0.7% of GNI to increase their assistance. Denmark will continue in the absolute lead in development assistance, with Denmark's assistance expected to be around 0.9% of GNI at factor cost in 2003. 7.1.2 New and additional assistance fundsBilateral action Denmark is at the leading edge with respect to making funds available for environmental action in the developing countries and in Central and Eastern Europe. It makes funds available partly through assistance under the facility for assistance to developing countries, which, as mentioned in the foregoing, has combating poverty in the developing countries as its main objective, and partly through the establishment of the Environment, Peace and Stability Facility (MIFRESTA) as an element of the follow-up on the Rio Conference in 1992. Through the latter, considerable funds have been spent on environmental action in developing countries, Central and European countries and the Arctic since 1993. Under MIFRESTA, Denmark is also engaged in the refugee area and prevention of conflict. In the poorest of the developing countries, assistance is aimed particularly at relieving povertyrelated pressure on the environment and nature, and in close cooperation with the recipient countries, Denmark provides considerable assistance to areas of relevance to sustainable development. This applies, for example, to the drinking-water area, where the action is helping to ensure millions of poor people access to water and to protect sources of water - e.g. by tree planning and by building up capacity for sustainable management. In the energy area Denmark provides support for sustainable energy supply - e.g. supporting poor women in planting trees for fuel, which provides the women with an income and at the same time, protects the environment. Within nature resources, Denmark is working to strengthen sustainable management and production with a view to preventing soil exhaustion and desertification. In the richer developing countries with growing economic activity, the assistance is aimed at helping the countries with environment and nature protection, primarily by strengthening their own capacity to solve the problems and by increasing environmental awareness. Table 7.1
Denmark's special environmental assistance under the MIFRESTA Facility increased up to 2002. Since then, however, this assistance has been considerably reduced because of increased requirements to the recipient countries to take more responsibility for the action, and the number of countries that can receive this assistance has been cut. The MIFRESTA countries are now Botswana, South Africa, Namibia, Mozambique,Tanzania,Vietnam, Cambodia,Thailand, and Malaysia, while assistance to Swaziland, Lesotho, Malawi, Zimbabwe, Zambia, and Laos has been cut altogether. Overall, Denmark will continue to provide extensive assistance for the benefit of the environment in the developing countries, since it is estimated that more than 15% of the facility for assistance to developing countries is spent on environmental assistance. Table 7.2
Multilateral action Denmark has worked - mainly through the EU - for binding and effective regulation of international environmental problems through the regional and global environment conventions. This applies, for example, to the conventions on biodiversity, climate change, combating desertification, the Basel Convention on cross-border transportation of hazardous waste and the conventions regulating chemicals, the Stockholm Convention on Persistent Organic Pollutants and the IMO Convention on toxic primers. Denmark has worked to get the conventions coordinated and enforced effectively and for the precautionary principle to have a central role in the rules. Denmark is a considerable contributor to the Montreal Protocol's fund for financing the phasing-out of ozonedepleting substances in developing countries. In addition, Denmark supports sustainable energy through socalled 'trust fund contributions' to the World Bank and the Asian Development Bank. Denmark's contribution to sustainable development includes considerable support for international organisations, particularly the UN system, in which all countries in the world participate on an equal footing. Here, Denmark is working to strengthen the Commission for Sustainable Development, CSD. Denmark is also working to make the UN more efficient so that the division of work between the organisations becomes better and overlapping is avoided. In the environment area, Denmark is working to strengthen the Global Environment Facility (GEF) financially and organisationally. The Danish contribution to GEF's replenishment for the years 2002-2005, the largest to date, is about 50% larger than in the previous replenishment. Denmark, together with other EU Member States, has made an extra, voluntary contribution to the third replenishment. Table 7.7
Table 7.8
The least developed countries are among the countries that are most vulnerable to climate change. Denmark therefore attaches particular importance to helping these countries adapt to climate change. For this reason, in 2002 Denmark made its first contribution of DKK 11.4 mill. to the fund for the least developed countries (the LDC Fund) under the Climate Convention. The contribution is intended to finance the least developed countries' work with National Adaptation Plans of Action (NAPAs). 7.1.3 Assistance through the private sectorDenmark has the following assistance instruments and measures for assistance to developing countries through the private sector: Mixed credits Mixed credits can be provided in connection with projects within both the public and the private sector. Restricted mixed credits are interestfree loans for development projects in credit-worthy developing countries with per capita GNP of not more than USD 2,380 (2002/2003) and are thus not reserved for programme cooperation countries. The loans are made from a Danish bank to a credit-worthy borrower in the recipient country. The interest expense, export credit premium, etc. are paid via the assistance funds. The project's assistance relevance is evaluated on the basis of Danida's ordinary rules for project evaluation. In the period 1997-2001 assistance was granted with mixed credits for 75 projects with a total contract sum of DKK 3.6 bill. and a grant for interest payments, export credit premium, premium etc., totalling DKK 1.4 bill. (see table 7.9). Approximately one fifth of these projects concern renewable energy - particularly wind turbines. In addition to the existing restricted mixed credit scheme, a new scheme - for unrestricted mixed credits - was introduced in 2002. The unrestricted scheme largely corresponds to the existing restricted scheme. The main difference between the two is that the support possibilities in the unrestricted scheme are not limited to Danish suppliers and that there is no requirement concerning the origin of the supplies. Besides this, the unrestricted scheme can only be used in Denmark's programme cooperation countries and in South Africa. Table 7.9
Denmark supports cooperation between the private sector in the recipient countries and in Denmark, including - particularly - cooperation projects between companies. Some of the projects are environmentrelated, e.g. projects relating to renewable energy and energy saving through transfer of cleaner technologies. Table 7.10 shows the support provided for these projects. Table 7.10
7.1.4 Assistance to developing countries that are particularly vulnerable to climate changesSmall Island Development States (SIDS) are particularly vulnerable to global environmental impacts, including climate change, and Denmark attaches great importance to supporting SIDS in accordance with Agenda 21 and the Barbados Action Plan. At the UN's special general assembly in September 1999 on these countries Denmark emphasised the prioritisation of the poorest developing countries among SIDS and weighting action in favour of women and the poorest target groups. In 1999 Denmark held a large NGO conference on renewable energy and small island states. In addition, Denmark provides support for SIDS through multilateral assistance to regional projects in the climate and energy areas and to projects on the Maldives, partly through the regional organisation "South Pacific Regional Environment Programme" (SPREP) and partly through UNEP. From 1998 to 2002 Danida supported a SPREP project on knowledge and capacity building in the climate area for governments, NGOs, and regional organisations on the Pacific islands. In addition, Danida is financing a supplementary capacity building project that UNEP is implementing on wind and other renewable energy technology in the electricity systems on the Pacific islands. In 2003 a new project on sustainable energy is being planned for the benefit of SIDS. 7.1.5 Activities in connection with technology transfer Examples of Danish-supported activities leading to transfer of technology include the energy sector in Malaysia and the establishment of a large wind farm in Egypt. The main purpose of the Danish support for the energy sector in Malaysia is to help the country develop a strategy for sustainable energy and identify ways of increasing energy efficiency. The project in Egypt has included support for the establishment of a wind farm in the Red Sea area with a capacity of 60 MW. This is one of the largest plants of its kind in the developing countries. More information on these projects is given in Appendix C. Table 7.12
7.2 Cooperation with Central and Eastern Europe7.2.1 MIFRESTA FacilitySince 1989 Denmark has been supporting the Central and East European countries' efforts to build up well-functioning democracies, which are now, after a number of turbulent years, characterised by economic growth and ever-stronger democratic institutions. The Danish assistance programme for Central and Eastern Europe has played an essential role in this process. Environmental activities have long constituted by far the largest part of all Danish assistance to Central and Eastern Europe. DANCEE has made grants for a number of projects aimed at reducing energy consumption and CO2 emissions. The total reduction of CO2 emissions through already completed and ongoing projects is now estimated to be about 0.75 million tonnes per year. Table 7.12 shows the main action areas. Table 7.13
The Danish Environmental Investment Facility for Central and Eastern Europe is contributing to a number of environmental projects in Central and Eastern Europe. The contributions, which are shown in table 7.14, are made as share capital or project loans and can thus not be regarded as real development assistance. 7.2.2 Strategy for Danish assistance to Central and Eastern Europe 2002-2003In April 2002 the government presented its strategy for Danish assistance to Central and Eastern Europe in the years 2002-2003. DKK 700 mill. has been earmarked for environmental projects in the years in question, including DKK 130 mill. for Joint Implementation. Under the previous environmental support programme for Central and Eastern Europe, projects were implemented that have in all resulted in CO2 reductions of about 0.75 million tonnes per year. Cooperation agreements have been entered into with Slovakia and Rumania on cooperation with a view to Joint Implementation projects and negotiations on cooperation agreements have also been held with Estonia, Latvia, Russia, Ukraine, Poland, and the Czech Republic. The planned action in 2002-2003 includes projects that will result in a considerable reduction in CO2 emissions, and Denmark will seek to credit this to the Danish climate account. Further agreements are expected to be entered into in 2003 with, among other countries, Rumania, Slovakia and Poland. In addition, the countries will be provided with technical assistance in building up the capacity that will be needed to enter into Joint Implementation projects.
8 Research and systematic observation8.1 Climate research and observations in generalResearch and observations within climate in the broad sense of the word take place at a number of institutes and organisations and cover a wide range of disciplines from natural science to evaluation of instruments and sociological aspects. Denmark's Meteorological Institute (DMI) carries out observations of climate parameters (atmosphere and ocean) under the World Metrological Organisation's (WMO) programmes and sub-programmes:World Weather Watch Programme (WWW), Global Atmosphere Watch (GAW), Global Observing System (GOS), Global Climate Observing System (GCOS) and Global Ocean Observing System (GOOS). Together with climate research, climate observations have been one of the DMI's main tasks for more than 125 years, with measurement, theory, and modelling. The establishment of the Danish Climate Center at the DMI in 1998 strengthened the area, and raised its public profile in national and international cooperation. Danish research competence concerning the physical expressions of past climate changes is to be found particularly at the Geological Survey of Greenland and Denmark (GEUS), the University of Copenhagen (KU) and Århus University. GEUS also has competencies in glaciological studies of the Greenland ice cap and the ice cap's interaction with climate change and in the effect of climate change on the water cycle in nature. The Geophysical Department and the Geological Institute at KU and the Geological Institute at Århus University have very great expertise in palaeoclimate data, and the climate group at KU is known worldwide for its ice core drilling and analyses. Besides research on the climate system, the Institute's climate-related research includes research concerning the driving forces for emissions of greenhouse gases and their impact on the environment, the state of the physical, chemical and biological environment, effects of climate change and society's possibilities for response and regulation. Denmark's National Environmental Research Institute (NERI), the Danish Forestry and Landscape Research Institute (FSL), the Danish Institute of Agricultural Sciences and Risø National Laboratory are all involved in these climate-related fields of research. In addition, several of Denmark's universities work on different aspects of climate research. The DMI has published an overview, parts of which describe current Danish research on climate changes1. It is on the basis of research competencies in the above-mentioned areas that Denmark also participates actively in IPCC's work. For example, Danish authors have been involved in IPCC's evaluation reports. The Copenhagen Global Change Initiative (COGCI) is a recently established and formalised cooperation in the form of a research network and a PhD school between three Danish institutions (GEUS, DMI, and NERI) and the University of Copenhagen. The COGCI covers all relevant scientific and interdisciplinary disciplines within global, regional, and local environmental impacts and climate problems. Danish climate research contributes to a wide range of international projects under the World Climate Research Programme, such as the Arctic Climate System Study (ACSYS), Climate Variability and Predictability (CLIVAR), the Global Energy and Water Cycle Experiment (GEWEX), Stratospheric Processes and their Role in Climate (SPARC) and the World Ocean Circulation Experiment (WOCE). 8.2 Research8.2.1 Research policy and fundingClimate-related research in Denmark is characterised by having grown up within an already existing framework as a natural development of institutions' activities. Denmark has not previously had a general national research programme for climate changes and global changes. However, as follow-up on Climate 2012, a committee was appointed to look at the possibilities for improving coordination of Danish research work on climate. This committee completed its work in December 2002. The work consisted primarily in mapping Danish climate research2 and making recommendations on that basis. Mapping was largely based on a questionnaire-based survey in which all known research centres with climate or climate-related research were contacted. Besides the narrowly focused scientific climate research, the survey has provided information on a broad section of climate-related research in Denmark. The mapping exercise showed that there is great diversity in relatively extensive climate-relevant research. The research is primarily concentrated on basic knowledge, consequences of climate change and mitigation of manmade climate change, whereas there has been very little research in adaptation to climate change. Table 8.1 The research is funded by the institutions' basic grants, programme grants, and the EU Commission's framework programmes for research and technological development, and by the Danish research councils. In the period 1998 to 2001 Danish climate research increased steadily, from 172 man-years in 1998 to 189 man-years in 2001. The budget increased correspondingly from DKK 94 million in 1998 to DKK 114 million in 2001, with foreign funding accounting for just under 30%. Besides the resources shown in table 8.1, a number of players are working with activities related to climate research, including activities under the Danish Energy Research Programme, the Nordic Energy Research Programme, PSO funds and Risø National Laboratory's Wind Energy Department, see section 8.2.6. In 2001 these spent DKK 379 mill. on activities indirectly or partially related to activities concerning mitigation of man-made climate changes. On the basis of the mapping exercise, the committee recommended a general, combined evaluation to determine which areas within climate research should receive larger grants from the government research councils or from other public support schemes. In addition, the committee presented the following proposals for special action areas to strengthen the entire Danish research in the area:
Lastly, the committee's research representatives proposed that more attention be paid in future to interdisciplinary cooperation, building up national and international networks, and disseminating the results, and that climate research be given a clearer place in the government's research policy. The government will consider the possibilities for following the committee's recommendations. Danish climate-related research is described in detail in the following sections, while a number of ongoing research projects are listed in Appendix D. 8.2.2 Climate processes and studies including palaeoclimatic studiesAt the DMI work is going on within atmospheric and coupled atmospheric oceanic processes, which are important in connection with global climate change. These process studies, which are going on in several international projects, include natural atmospheric oceanic interplay on time scales from years to decades and the main processes of importance for deep water formation in the North Atlantic. Through assimilation of atmospheric reanalyses in atmospheric models, several studies are being carried out of atmospheric processes that are important partly for developing improved atmospheric models and partly for detecting changes in the external climate impacts. In addition, trends and variations in the latest tropospheric temperature observations from satellites (primarily MSU data) and radio soundings are being analysed and compared. At the DMI work is going on to improve models for describing the thinning of the stratospheric ozone layer. This area is important, not only in relation to the Vienna Convention concerning protection of the stratosphere's ozone layer, but also in a climate context, because there is interaction with the greenhouse effect. The DMI has participated in all major European-American Arctic ozone campaigns in the 1990s, such as EASOE, SESAME,THESEO, and THESEO-2000/SOLVE. The research is based on analyses of a broad range of available observations compared with analyses of the meteorological conditions in the stratosphere. It includes analyses of the dispersal of ozone-depleted air from the Polar regions to intermediate latitudes, experimental and theoretical model work concerning the formation of polar-stratospheric clouds, and modelling of the propagation of localised mountain waves. The work, which is receiving support from the EU Commission's framework research programmes, is aimed at better understanding and modelling of the processes that lead to chemical depletion of the ozone layer. The Geophysical Department under the Niels Bohr Institute for Astronomy, Physics and Geophysics at the University of Copenhagen is working mainly on global and general problems, such as the natural variability of the climate in all time scales and the role of basic physical/chemical processes in the climate system. Examples of projects are the international ice core projects, the aim of which is to analyse ice cores through Greenland's ice cap in order to obtain a climate series that covers as long a period of time as possible and to obtain information about the end of the last ice age 11,500 years ago, and about the last warm period 130,000 years ago. At Odense University research is going on within the areas of the climate system's stability, the role of the ocean in the climate system and the chemical and biological development of the atmosphere and the ocean. The newly established Center for Planet Research undertakes climate research in a more general sense - for example, it studies ice deposits not only on earth but also in the solar system. GEUS works with the physical expressions of past climate changes, including ecosystems' response, temperature variations, changes in precipitation and rises in water level. Another research topic is past variations in the circulation of the North Atlantic sea currents and their importance for climate changes. GEUS also works with mass balance studies of Greenland's ice cap, including its interaction with climate change and its effect on changes in water level. 8.2.3 Climate modelling and the climate of the futureWith substantial support from the European Commission, the DMI/Denmark's Climate Center are working closely together with research institutions in Europe on analyses of the climatic consequences of increased greenhouse effect, depletion of the stratospheric ozone layer and variations in solar activity. The main emphasis is on Denmark and the European region, but global research is also being carried out. The work includes both developing models and using the models for scenario calculations of the climate of the future. The models include:
In 2000 both global and regional scenario calculations were carried out3 based on IPCC's so-called SRES emission scenarios - more specifically, scenarios A2 and B2, and the results have been used in the IPCC's Third Assessment Report. For Denmark it is particularly changes in (extreme) precipitation, soil moisture and storm activity that are important. For Greenland it is particularly changes in the simulated snow accumulation on the ice cap that are of interest. In the European climate project PRUDENCE, which is being coordinated by the DMI, researchers are working with several climate models to reduce and quantify the uncertainty in climate projections and interpretation of the results in relation to European strategies for mitigating climate change and adapting to it. The research on ozone as a greenhouse gas includes the influence of ozone on circulation in the stratosphere, together with radiation forcing and climate effects caused by changes in the ozone concentration. In the research in this area, use is made of a global climate model and a more simple radiation convection model. Research at the Geophysical Department of the University of Copenhagen includes experimental/field-related, theoretical, and modelling aspects and helps to indicate methods that can be used for evaluating the climate of the future. 8.2.4 Effects of climate changeThe effects of climate change on nature and ecosystems are covered by research at GEUS, NERI, the Danish Forest and Landscape Research Center (FSL), the Danish Institute of Agricultural Sciences and Risø National Laboratory. FSL carries out research on the direct effect of changed CO2 concentration on Danish forests through its cooperation with the Royal Veterinary and Agricultural University. NERI has research competence concerning toleration limits for air pollution for particularly sensitive ecosystems on agricultural land. NERI works with climate change in Greenland, where adverse effects can be expected. NERI is carrying out a standardised biological/ecological monitoring programme covering a broad spectrum of processes, fauna, and flora. In connection with this project the institute is carrying out research projects aimed at increasing knowledge of basic Arctic ecosystems. In the last five years NERI has built up competence focused on the Arctic marine ecosystem's function and dynamics and is investigating an Arctic fjord system and, within that, relationships between production and nutrient conversion. GEUS has competence concerning long-term variations in ecosystems in Denmark and Greenland and on the Faroe Islands caused by the climate. The institute is investigating how the ecosystems react to climate change in lakes and marine environments in Denmark and Greenland and in forests in Scandinavia. It also registers changes in sea level and their effect on the water cycle, including the formation of groundwater. The Danish Institute of Agricultural Sciences works with the interaction of climate and agriculture, including effects of climate and atmospheric CO2 on processes in the soilplant system. Other aspects being studied include factors affecting greenhouse gas emissions from agriculture, e.g. energy consumption in the agricultural sector, biomass for energy purposes, production and handling of manure, biogas, and NH3 volatilization, and greenhouse gases in relation to feeding strategies, manure handling, and soil tillage. Risø National Laboratory's work includes a number of sub-projects on effects of climate change in developing countries, where the centre's activities include both analyses of vulnerability to climate change and adaptation strategies. The activities cover the energy, industrial, forestry, agricultural, transport, and waste sectors. There is not at the present time special competence concerning the effects on humans and their conditions of life and health, which are particularly relevant in those areas in the world where dramatic climate effects are expected/seen. An element of NERI's work programme for 2000 and 2001 was a pilot study of the equality problem between developing countries and industrial countries. The Geographical Institute at the University of Copenhagen is doing research on soil-forming processes in relation to climate and vegetation that are of significance for, amongst other things, the exchange of greenhouse gases between soil and the atmosphere. 8.2.5 Economic research, including evaluation of climate change and possibilities for mitigationIt is important to take account of the economic consequences of the different ways of reducing greenhouse gas emissions. NERI's Center for Analysis of Environment, Economy and Society has general competence in setting up and evaluating mechanisms for reducing emissions and special competence within the agricultural, energy and transport sectors. In addition, it possesses general knowledge of the different aspects of the Kyoto Protocol, including research competence concerning Joint Implementation. Risø National Laboratory is involved in various research activities, primarily relating to policy and mechanisms for reducing greenhouse gas emissions, and relating to emission scenarios for greenhouse gases. The activities include development and implementation of international method standards for cost and sustainability analyses of reduction policies, discussion and testing of baseline approaches and various project and sector studies for the energy, transport, and agricultural sectors. The research activities have also included support for the Climate Secretariat and capacity and training programmes in developing countries. In addition, Risø has research activities concerning the Kyoto Protocol's flexible mechanisms, Emission Trading (ET), Joint Implementation (JI) and Clean Development Mechanism (CDM). Research at Aarhus University is concentrated on the regulatory aspects of the climate problem. The Center for Social Science Research on the Environment (CeSam) at Aarhus University thus has general competence in research in mechanisms - particularly in the effects of economic instruments (taxes and quotas) and voluntary agreements. In addition, the centre has thorough knowledge of environment and energy policy, including climate policy in the industrialised countries. The University of Southern Denmark in Odense carries out research in climatic, ecological and anthropogenic impacts on marine environments, particularly the North Sea and the Baltic Sea in the period 1500-2000. At the University of Copenhagen the main focus of climate research is the scientific aspects, but research is also being conducted in the climate field in an economic context, at the Economic Institute, for example. At Roskilde University Center, research is going on concerning scenario building within climatestabilising policies, together with life cycle analyses as a tool in economic evaluation of climate-stabilising strategies. 8.2.6 Research and development of technologies to reduce greenhouse gas emissions and to adapt to climate changeAt the Technical University of Denmark (DTU), the energy/environment group and the group for urban ecology base their research on sustainable energy development and sustainable urban change, with energy savings and renewable energy as central parameters. The Energy Research Programme (EFP) has hitherto supported a large number of research and development activities in the energy field. The activities have ranged all the way from social science research on the interaction between the energy sector and the rest of society to research in such advanced energy technologies as super conductors and fuel cells. In 2002 funding for the programme was reduced from the previous annual sum of between DKK 200 mill. and DKK 250 mill., and at the same time, the action areas were narrowed. However, the energy research effort will increase again from 2003, mainly within renewable energy, with a pool administered under the Ministry of Science,Technology and Innovation. The EFP contributes to Danish energy research with a long-term perspective, and industry is also involved. Statistics on research projects show that private companies, together with energy and research institutions, contribute almost 50% of the financial support for the research projects. NERI concerns itself with the main forces behind greenhouse gas emissions from the energy sector, the agricultural sector, and the transport sector. FSL has competence in forestry, afforestation, etc. Together, these two institutions cover the aspects of land use in the open countryside for agricultural purposes, forestry and nature. In this connection, both institutions are studying problems related to use of biomass from agriculture and forestry as an energy source. NERI makes general inventories of atmospheric emissions from all sectors and activities, including the greenhouse gases. The institution has special research competence in inventories from the agricultural sector, the transport sector, and the energy sector. FSL seeks generally to quantify how forestry and changes in land use in relation to forests affect the forest ecosystems' carbon sinks and thus the potential binding of CO2 in biomass and soil. NERI also has research competence in modelling of the dispersal of greenhouse gases locally and regionally, with special focus on Denmark, Europe, and Greenland. The Department for Atmospheric Environment is developing a CO2 model (DEHM) for dispersal, transport, and surface movements. The model can be used to determine the size of sources and drains for CO2 in Europe over specific areas and for estimating whether these areas comply with the Kyoto Protocol. GEUS is researching impacts from earlier eras on the environment, and the driving forces for natural climate variations in long-term perspectives. In cooperation with seven other countries, GEUS is the project manager for the EU-funded GESTCO project, in which the possibilities for finding geological storage possibilities near the European power stations and large industrial CO2 point sources are being studied. Also in this project a technical-economic model is being developed for planning and price calculations of different combinations of sources of CO2 emissions, transport, and types of geological stores. Several geological formations in Denmark are known to be suitable for deposition. Publication of the results will be followed up by public hearings. GEUS is also participating in the international research project SACS, in which CO2 deposition from the Norwegian Sleipner gas field is being further developed. GEUS is studying the geological conditions for the store, including the spread of the sand formation, the tightness of the clay seal and the chemical effects of storing CO2 in the form of carbonic acid where the acidity is very low. Under the Danish Electricity Supply Act, the system operator is responsible for ensuring the research and development projects that are needed for use of environmentally sound electricity production technologies. In 2000 and 2001 a sum of around DKK 100 mill. per year was used for this purpose, including research and development within wind power, biomass and waste, other renewable energy, CHP and use of gas and system fitting. Risø National Laboratory is carrying out research projects on the driving forces, emissions and possibilities for reduction, particularly in the developing countries. Research at the Danish Institute of Agricultural Sciences focuses on the agricultural sector's possibilities for adapting to climate change by changing the cultivation system, including changes in fertilisation and the use of pesticides and adapting soil tillage methods. The aim is to develop adaptation options that also reduce greenhouse gas emissions from the sector. 8.3 Systematic climate observations8.3.1 Atmospheric climate observations, including measurements of the atmosphere's compositionSince its establishment in 1872 the DMI has monitored the main climate parameters. In the climate monitoring programme classic methods of measurement are used and new, satellite-based methods of observation are being developed. The DMI operates around 200 automatic measuring stations in the Kingdom (Denmark, Greenland and the Faroe Islands) with a broad measuring programme ranging from automatic water-level or precipitation stations that measure only a single parameter to stations with a full measuring programme, including automatic cloud-height detectors and weather-type detectors. Since 2001 a separate network for climate observations has not been operated because of technological convergence between the weather networks and the climate networks and a need to rationalise the measuring network. Table 8.2
The purpose is to achieve convergence between the different types of stations so that the number of station types and spare parts can be reduced as much as possible without loss of quality. To collect precipitation data the DMI also operates a network of 500 manual precipitation stations, which are mainly used to map the precipitation climatology. 100 stations report daily via an automatic telephone service called "Tast-Selv", and 400 monthly by postcard. Besides being used in national programmes, the observations are part of Denmark's international contribution in the form of observation components from Danish territory to the worldwide meteorological observation network WWW (World Weather Watch), GCOS (Global Climate Observing System), and other international programmes for mapping weather and climate. Table 8.3.
The meteorological observations are stored in the DMI's database, and observations from many Danish stations are available in electronic form right back to 1872, water level measures from 1890 and measurements of sea surface temperature from 1931. In 2001 the number of daily observations was 75,000, and the total number of observations in the database is around 245,000,000. The meteorological observation systems that are of most interest in a climate context are:
Each of these systems is described in the following, together with the DMI's stratospheric observations and oceanographic observations. The surface observation network For historical and practical reasons, the surface observation network consists of many different types of station. Except in the case of the manual precipitation and hours of sun stations, the stations have been gradually automated since the 1970s at an increasing rate, and by the end of 2000, Denmark had an almost 100% automated network of weather stations. Table 8.3 shows the station network. DMI is receiving a growing number of observations from cooperation partners in all parts of the Kingdom, so these are included in table 8.3. Besides the observations from the Danish land areas, the DMI has an observation agreement with about 50 Danish, Greenlandic and Faroese ships, which carry out systematic observations in the North Sea, the Baltic Sea, the North Atlantic and the waters around Denmark. In addition, Denmark is a partner in the EGOS cooperation on collection of weather observations from drifting weather buoys in the North Atlantic, since the DMI has strategically well placed satellite reception facilities in Kangerlussuaq (Greenland) and in Copenhagen. The siting of weather stations in Denmark and Greenland and on the Faroe Islands, together with precipitation stations in Denmark, is shown in Appendix E (the GCOS Report). Radio sounding network In radio sounding, a small, fully automatic weather station is sent up by balloon. The balloon can reach a height of about 35 kilometres, and all the way up it sends observations of temperature, pressure, humidity, and wind velocity via radio to a receiving station. Radio soundings provide measurement of the atmosphere's vertical profile for use in analyses of the condition of the atmosphere. They also enable measurement of ozone and radioactivity. The DMI operates radiosounding stations in Copenhagen, in Thorshavn on the Faroe Islands and in Danmarkshavn, Illoqqortoormiit, Tasiilaq, Narsarsuaq, and Aasiaat in Greenland. Soundings are also received from two so-called ASAP (Automated Shipboard Aerological Programme) containers, which are portable radio sounding stations designed for use on ships. The DMI has had an agreement for many years with a Greenland shipping company on ship-borne radio soundings in the North Sea and the North Atlantic. The radio sounding stations and the ASAP units take two daily soundings, although the ASAP units do not take a sounding if they are near a land radio sounding station, such as the one in Thorshavn. The total number of soundings per year is in the order of 5,800. Weather radar network With radars in Sindal and on Stevns, Rømø and Bornholm, Denmark's network of weather radars provides almost 100% coverage. It also has an extremely closely meshed network of land-based precipitation stations. The weather radar network has supremely high spatial resolution and is therefore able to provide precipitation climatological information with a very high degree of detail nationally, regionally, and locally. By calibrating radar data against surfacebased point-precipitation measurements, the latest research results show that good absolute accuracy can be achieved. The present radar network has a data frequency of six data sets per hour and the spatial resolution is 2x2 km2. Satellite data Denmark contributes to spacebased observations through membership of the European space organisation ESA and the European meteorological satellite organisation EUMETSAT, and DMI has facilities for receiving satellite data in Denmark and Greenland. In cooperation with EUMETSAT, NERI is managing the development of a so-called satellite application facility (SAF) for use of GPS data for weather and climate monitoring and is also participating in the development of SAFs for oceanography and sea ice, together with ozone and UV radiation. 8.3.2 The ice observation serviceThe DMI is responsible for systematic monitoring of the ice conditions in the waters around Greenland. Observations of the ice conditions have been collected for about 125 years, and there is a very large quantity of data in graphic form in the way of monthly surveys, ice maps, etc. Since 1956 the waters south of Kap Farvel, in particular, have been intensively monitored with a view to making shipping in the area safer. Ice maps are prepared several times a week with detailed information on relevant ice conditions. All new ice maps are in vector-graphic form. Since 2000 weekly maps have been prepared showing the ice conditions all the way round Greenland. The maps are based on satellite data and are essentially an automatically produced product that is primarily intended as a basis for analyses of climatic conditions for Greenland and the surrounding waters. 8.3.3 Stratospheric observationsThe DMI monitors the stratospheric ozone layer, taking daily earthbased measurements of the thickness of the ozone layer from Copenhagen and Kangerlussuaq (Søndre Strømfjord) with Brewer spectrometers, together with daily measurements from Pituffik (Thule Air Base) in the spring and autumn months with a SAOZ spectrometer. The DMI also takes weekly measurements of the vertical ozone profile by means of balloon-borne soundings from Illoqqortoormiit. The measurements are reported to the databases under Network for the Detection of Stratospheric Change (NDSC) and World Ozone and UV-radiation Data Center under the WMO programme Global Atmosphere Watch. Ozone soundings are also carried out on a campaign basis from Pituffik and Illoqqortoormiut in the winter and spring months, often as an element of major international campaigns. Balloon-borne experiments are also going on for studies of polarstratospheric clouds from Greenland and Scandinavia. Data from the research campaigns are reported to the Pan-European data centre at NILU in Norway. The DMI's stratospheric observatories in Pituffik and Kangerlussuaq are primary and secondary Arctic stations, respectively, in Network for the Detection of Stratospheric Change, a worldwide network of measuring stations equipped with standardised instrumentation of verified high quality for monitoring the condition of the stratosphere and the processes that lead to chemical depletion of the ozone layer. Besides ozone and NO2 observations, the DMI in Pituffik takes measurements of the level of UV-B radiation. Besides the DMI's instrumentation, the NDCS stations include lidars for measuring stratospheric aerosol and cloud particles (Italy and USA) and an infrared spectrometer (USA) for measuring a wide range of stratospheric trace substances. 8.3.4 Reanalyses and climate databasesThe DMI cooperates with the Pan European meteorological forecasting centre in the UK, European Centre for Medium-Range Weather Forecasts, on building up and using socalled global reanalyses, which are a fundamental set of data for understanding climatic variations and changes based on all measurements globally over a 40-year period. In addition, databases of the climate trend in the past 100 years or so are created and maintained, cf. 8.3.1. 8.3.5 Oceanographic climate observationsTogether with the Danish Coast Directorate, the DMI monitors the water level in a number of Danish localities. In cooperation with the Greenland Institute of Natural Resources, the DMI carries out annual oceanographic observations on standard sections of the west coast of Greenland for the purpose of monitoring climate changes in the Greenland marine environment with a view to use in fishery evaluations. The DMI also participates in special measuring campaigns in, for example, the North Atlantic. For instance, in 1999, the DMI took over the management of the research vessel DANA's expedition in the Greenland Sea, the purpose of which was to investigate the importance of this sea for global ocean circulation and its influence on the global climate. 8.3.6 Terrestrial observations related to climate changes Monitoring of snow cover, sea ice and surface radiation is reported in sections 8.3.1 and 8.3.2. Denmark does not carry out further terrestrial observations that can be related to climate change, but Denmark's climate related research (cf. 8.2) includes monitoring and studying the effect of terrestrial conditions. 8.3.7 Development assistance for establishment and maintenance of observation and monitoring systems Since September 1997, the DMI has participated in a development project together with the Ghanaian meteorological institute (Meteorological Services Department - MSD). The purpose of the project includes reestablishing a network of meteorological stations in the country, thereby ensuring collection of data. At the same time, work is going on to improve communication and use of the collected data. According to plan, the project will run until the end of 2003. At the end of the project, MSD is intended to have an efficient network of around 300 observation stations registering the usual meteorological parameters. The DMI is also participating in the project "Use of climatic seasonal forecasts to improve cultivation strategies for crops in West Africa". The purpose of this project is to examine the possibilities for adapting cultivation practice for a selected agricultural crop (peanuts) in Ghana, using the best available seasonal forecasts for the climate. The project is funded by the Council for Developing Country Research (RUF). Finally, the DMI is participating in a knowledge-building initiative within use of regional climate scenarios in developing countries.
9 Education, training and public awareness
In Denmark there is an ongoing public debate in the media and elsewhere on the anthropogenic greenhouse effect, its extent, and the political reaction in the form of policies and measures. In 2002 the government published its strategy for sustainable development. The Danish climate policy must be seen in the light of the action to make the development of Danish society sustainable. The strategy includes involvement of the public and transparency concerning the basis for decisions and analyses. Denmark has a long tradition for involving the public, and in the environmental area this was followed up with an international agreement - the Århus Convention from 1998. In the international UN negotiations on a common effort to mitigate the effect of climate changes, both Danish industry, and green and developmentoriented organisations were represented in the Danish delegation. The websites of the Ministry of Environment (http://www.mim.dk/), the Danish Environmental Protection Agency (www.mst.dk), the Ministry of Finance (www.fm.dk), the Ministry of Economic and Business Affairs (www.oem.dk) and the Danish Energy Authority (www.ens.dk) provide considerable information about climate change and Denmark's policy in this area. The Danish Environmental Protection Agency has also initiated mapping of information obligations and activities in the climate area. The main purpose of the mapping project is to contribute to a basis for decisions on future information activities in the climate area on the basis of Denmark's formal commitments, the initiatives of Denmark and others, and general activities up to the present time. 9.1 Education and postgraduate education programmesClimate change is a central theme at Copenhagen Global Change Initiative (COGCI), which is a PhD school and research network established in cooperation between the University of Copenhagen, the DMI, NERI, and GEUS. The school has 25 PhD students registered at present. The programme comprises general and specialist courses, together with seminars and theme days. Seminars and theme days are open to the public, and plans are in hand to offer the courses to other institutes and the business community as supplementary training. The universities disseminate widely the result of research - for example, the Niels Bohr Institute's activities are published at the website http://www.fys.ku.dk/hco/presse/For midling2002.htm. A large part of this work concerns climate, both specifically and more generally. The DMI arranges lectures for, for example, upper secondary school pupils, teachers, researchers, and other interested persons. In addition, employees from a number of institutions participated in the Danish Natural Science Festival in 1998 and 2000, holding lectures around the country. For upper secondary school pupils and pupils taking the higher preparatory examination, the Ministry of Environment, together with the Ministry of Foreign Affairs has prepared material for teaching about the environment. This project, which is called "The Global Environment" has climate as one of its main themes. The material is Internet-based (www.globalemiljoe.dk) and is supplemented by a textbook. In connection with the many projects initiated under the Danish Environmental Protection Agency's (DEPA) Programme for Cleaner Products, reports are required, and these are made publicly accessible. In addition, articles are prepared for various technical journals so that the relevant target groups learn about the results. 9.2. Climate informationThe DEPA website is regularly updated with the latest relevant information within the climate area, either directly in the form of press releases, documents, reports, etc. or through links to the actual players. NERI has prepared a number of reports. Technical Report No. 401 contains an evaluation of Denmark's need and possibilities for adapting to future climate changes. The report features on NERI's website www.dmu.dk. A number of NERI's reports on climate are also designed for use in the education sector, including Theme Report 29/1999 "Where does air pollution come from?" and Theme Report 31/2000 "CO2, where, why, how much?". The DMI's website, http://www.dmi.dk/, provides current and historical climate data, together with a thorough description of the climate system and climate processes and themes on new results from the international scientific literature. The DMI also communicates through lectures and popular articles in newspapers and trade journals, through books and series of reports, and at theme days and in the magazine KlimaNyt (Climate News), which is published electronically two to four times a year. In 2001 the DMI published the book "Climate Change Research - Danish Contributions", edited in cooperation with Risø National Laboratory and NERI. The book provides a general introduction to the problem of man-made climate changes and describes research projects and results at a number of institutions in Denmark. The reports, KlimaNyt and the climate book can be obtained at www.dmi.dk. IPCC's results in the "Third Assessment Report" (TAR) in Danish have been disseminated in part through publication of a book, "Global Warming - Mitigation and Adaptation". Another website of interest is http://www.glaciology.gfy.ku.dk/, which is regularly updated. 9.3 Danish participation in international climate activitiesThe DMI participates in a number of international projects with support primarily from the European Commission's framework research programmes. In addition, the Institute contributes to the IPCC's work. Partly in cooperation with the Max Planck Institut für Meteorologie in Hamburg, the DMI has carried out analyses of the development of climate for two of the IPCC's SRES emission scenarios with a coupled atmosphere ocean model system. These scenarios are available for effect studies in the IPCC's scenario database. Employees at the DMI have also participated in the preparation of the IPCC's Third Assessment Report (TAR) - one was coordinating author, another contributing author and several participated as expert reviewers. The Danish Institute of Agricultural Sciences has contributed to the IPCC through an EU Concerted Action concerning effects of climate changes and adaptation to a changed climate in Europe. Risø National Laboratory also participates at expert level in the IPCC. The UNEP Centre at Risø has contributed to the TAR WG III Report with five authors and a coordinating author. The UNEP Centre participates in a wide range of information activities in that connection with different policy possibilities in cooperation with the DMI, NERI, and others. NERI works in different ways to popularise and communicate the content of TAR, the latest research results on climate effects, etc. 9.4. Public campaignsCampaigns A number of initiatives are being carried out for companies and private households with a view to promoting environmentally sound behaviour, particularly for climate reasons and in relation to energy use. Denmark uses labelling schemes, printed material, information lines and media spots to increase public knowledge of possibilities for action and least environmentally harmful technology. In the last few years environment policy has increasingly focused on the fact that we all share responsibility for environmental problems and for helping to solve them. This strategy is now also penetrating in the transport sector, and in the last three to four years, two large nationwide environmental traffic campaigns have been implemented."We cycle to work" and "Environmental Traffic Week", which is an element in the European car-free day on 22 September and European Mobility Week, in which more than 1,000 towns all over Europe participated in 2002. In "We cycle to work" the Danish Cyclists' Federation has established good cooperation with many citizens and companies and has particularly communicated the health benefits of cycling as a form of transport. In "Environmental Traffic Week" the emphasis was on demonstrating more environmentfriendly transport habits (use the car less, buy an energy-efficient car, drive together with others, use the bike for short trips, use public transport as much as possible, etc.). Emphasis was also on discussing traffic habits with the public in open dialogue and without reproach. In this way greater public engagement in the cause of environmental traffic can be established and help to create greater understanding of new ways of organising urban transport systems. Another reason for the increased campaign and information activities is that a combination of measures affecting attitudes and behaviour and other forms of encouragement, such as economy and accessibility without a car are needed to promote more environment-friendly traffic habits. Evaluations1 show that both "We cycle to work" and the "Environmental Traffic Week" have had a good effect and have been well received by municipalities, interest and grassroots organisations, and companies, all of which were in charge of most of the actual activities. The Ministry of Transport and the Ministry of the Environment have so far provided funding of DKK 4-5 million for Environmental Traffic Week each year in order to support and co-fund the work of the municipalities. The present government co-funding ends in 2003, after which it will be up to the Danish municipalities themselves to finance any participation in European Mobility Week. In the years ahead the growing public focus on lifestyle diseases and obesity will probably provide good opportunities for marketing nonmotorised forms of transport, such as cycling and walking, in public health campaigns drawing peoples attention to the health benefits of using a bike more often, walking to the shops, leisure activities, etc.
Appendix A: Greenhouse gas inventories 1990-2001This appendix contains five tables summarising the results of the latest greenhouse gas inventories for Denmark 1990-2001 and tables showing the preliminary inventories of Greenland's CO2 emissions from energy use 1990-2001and the Faroe Islands' emission of CO2, methane (CH4) and nitrous oxide (N2O) 1990-2001. The tables have been reproduced from the annual report to the Climate Convention from April 2003 (The National Inventory Report - NIR, including the Common Reporting Format - CRF).
Table A.2 Table A.3 (10-3) Table A.4 (10-4) Table A.5 (10-5) Table A.6
Appendix B: Projections of Denmark's greenhouse gas emissions and removals up to 2017This appendix contains the result of the latest "with measures" projections of Denmark's emissions and removals of greenhouse gases published in Denmark's Greenhouse Gas Projections until 2012, an update including a preliminary projection until 2017, Environmental Project No. 764, Danish Environmental Protection Agency, 2003. "With measures" means that only the effects of implemented measures have been taken into account in the projections. The effects of further possible measures and their costs are described in chapter 4. The result for each greenhouse gas and the combined result are presented in tables showing the source and sector breakdown in the IPCC/UNFCCC CRF format, which is also used in connection with the annual reporting of the historical inventories of emissions and removals of greenhouse gases.
Table B.1 Table B.2 Table B.3 Table B.4 Table B.5 Table B.6 Table B.7
Appendix C: Description of selected programmes/projects for promotion and/or financing of technology transfer to other countriesPart I
Part II
Appendix D: List of current climaterelated research projectsThe Danish Meteorological Institute (DMI)The following research projects for the period 2002-2003 are being financed by the EU Commission's research programme EUMETSAT and national research councils and programmes.
Geological Surveys of Denmark and Greenland - GEUS
Aarhus University (Geological Institute)
Danish Institute of the Agricultural Sciences (DJF)
University of CopenhagenGeophysical Department Projects are in progress within the following areas:
Geological Institute
Geographic Institute
Institute of Molecular Biology
Institute of Chemistry. The Atmosphere Group
Botanical Institute
Risø National LaboratoryDepartment for Plant Research
Energy System Group
Department for Wind Energy
National Environmental Research Institute (NERI)Department of Marine Ecology
Department for Arctic Environment
Department for System Analysis
Department for Terrestrial Ecology, Soil ecology and Ecotoxicology
Department for Atmospheric Environment
Technical University of Denmark
Danish Forest and Landscape Research Institute (FSL)
Institute of Local Government Studies
The Royal Veterinary and Agricultural University
National Survey and Cadastre
Appendix E: Denmarkss report on systematic observations for the Global Climate Observing System (GCOS)Denmark's report on systematic climate observations for the Global Climate Observing System (GCOS) for the third national communication to the conference of the parties to the United Nations Framework Convention on Climate Change (UNFCCC)
Yearly mean Temperature, Denmark, 1873-2000 Chapter 1 Introduction Chapter
2 Meteorological and Atmospheric Observations Chapter 3
Oceanographic Observations Chapter 4 Terrestrial Observations Chapter 5 Space-based
Observing Chapter 6 Activities in Developing Countries relating to Observations.
Editor: Lillian Wester-Andersen (DMI) Chapter 1 IntroductionThis report is prepared to give a status on the Danish contribution to the systematic climate observations for the Global Climate Observing System (GCOS). The report is part of the Third National Communication to the Conference of the Parties to the United Nations Framework Convention on Climate Change (UNFCCC). Climate research and the generation of climate-related observations are carried out by various government departments in order for them to meet their responsibilities. Currently, no national plan exists for the whole area of climate research and observations. Many agencies in Denmark engage in the systematic observation of elements of the climate system. Invariably the capture, quality control and archiving of such data are designed to meet the integrated needs of these agencies, deriving from their overall missions. Typically the drivers for longterm systematic observation of environmental or ecological characteristics arise from an operational, regulatory or research need. Examples of the former are to be found in the capture of meteorological data for predictive and statistical services by the Danish Meteorological Institute (DMI). The resulting observation programmes tend to be long term, but the resulting individual data may be seen as perishable and focus might not always be on maintaining stability and reliability in the records. The general need for systematic and reliable time series is increasingly understood in the scientific community and incorporated in the collection and data handling procedures. In this report relevant climate observations for Denmark, Greenland and the Faroe Islands will be described. In general the data are available from the institution operating the observing station / collecting the data, but many can also be found on the web, for instance www.dmi.dk. Where data such as contributions to GCOS are submitted to the appropriate Data Centres, they are also available from these centres. Additionally, all meteorological data and products that are produced by WMO Members (national meteorological services) to the WMO programmes such as the WWW are available under the terms of WMO Resolution 40 (WMO policy and practice for the exchange of meteorological and related data and products including guidelines on relationships in commercial meteorological activities). Such data are "freely" available "without charge" (i.e. at no more cost than the cost of reproduction and delivery, without charge for the data and products themselves and with no condition on their use). Similarly hydrological data and products are covered under WMO Resolution 25. Further the IOC are expected to adopt a data policy which provides for free and open access to data that are collected, produced or exchanged as part of oceanographic programmes conducted in association with the IOC. Chapter 2 Meteorological and Atmospheric ObservationsDenmark participates fully in the GCOS Surface Network (GSN) and the GCOS Upper Air Network (GUAN), and in the Global Ozone Observing System (GO3OS) as part of the Global Atmosphere Watch (GAW). GCOS Surface Network / GSN Stations The designated 7 GSN stations in Denmark, Greenland and on the Faroe Islands are all run by DMI and consists of:
All of these currently meet the GCOS standard for surface observing. GCOS Upper Air Network / GUAN Stations Only one GUAN station is designated for Denmark, Greenland and the Faroe Islands and it is situated in Narsarsuaq, Greenland. The station is run by DMI and is operated to GCOS standard. A survey of the performance in 2000 shows that 92% of the soundings reached an altitude of 30 hPa. GCOS Global Atmospheric Watch / GAW Stations Denmark contributes to the Global Ozone Observing System (GO3OS) as part of the GAW programme with three stations in Greenland and one in Denmark. The stations in Kangerlussuaq (Greenland) and Copenhagen (Denmark) are equipped with Brewer spectrometers, the station in Pituffik (Greenland) is equipped with a Dobson and a SAOZ spectrometer and the station in Illoqqortoormiut (Greenland) is equipped with a SAOZ spectrometer. The spectrometer in Illoqqortoormiut is operated by Service d'Aeronomie (France) in cooperation with DMI while all other spectrometers are operated by DMI. All data are available from DMI. Table 1.
1 The Danish participation is in the GO3OS of GAW Other National and Meteorological and Atmospheric Observations: Surface Climatological/ Meteorological Network DMI operates and receives data from a network of approximately 100 automatic meteorological stations in Denmark, Greenland and on the Faroe Islands. Measurements are made in accordance with the WMO recommendations.
Figure 1: As from 2001 a special dedicated network of (manual) stations for climatological observations has been discontinued, due the convergence of the different network technologies. The objectives behind this decision are to eliminate human errors, to benefit from potential savings in the rationalisation and to reach a higher observation frequency. Climatological data are now obtained from the automatic network described above. Climatological data are collected to define the climate in Denmark, Greenland and on the Faroe Islands and to create a national database for a wide range of enquiries and research activities. Most climatological work involves the production of annual or monthly statistics including means, percentiles and standard deviations.
Figure 2:
Figure 3: Long records are needed to establish reliable averages and trends. In 2001 the daily inflow of data from Denmark, Greenland and the Faroe Islands was 75,000 and in all 245,000,000 observations are currently stored in the database. The observations are stored in a central database at DMI, where data from several meteorological stations are stored as far back as 1872. A monthly summary is prepared for three stations in Denmark, one on the Faroe Islands and 8 in Greenland on the CLIMAT format. These data are routinely submitted on the GTS. Rainfall Observing Network (Stations and Radar) The need for rainfall data is greater than what is generated from the overall surface climatological and meteorological network described in the above paragraph. In Denmark the rainfall network consists of approximately 575 stations. Roughly 75 of these provide continuous data on rainfall intensity. They are operated jointly by DMI and The Water Pollution Committee of the Society of Danish Engineers (SVK). The remaining 500 stations collect daily values on rainfall and from approximately 100 of these data are transmitted to DMI on a daily basis, whereas the remaining data are received as monthly sums.
Figure 4:
Figure 5: On the Faroe Islands a rainfall network of 22 stations collects daily information about the precipitation. Information on precipitation can also be obtained from weather radar data. In Denmark DMI runs a network of three weather radars which provides nearly 100% coverage. In the early part of 2002, an additional radar on the island of Bornholm will further improve this coverage. The network has an unsurpassed high spatial resolution, and hence provides very detailed climatological information about precipitation both on national, regional and local scale. By calibrating radar data against pointmeasurements of precipitation the latest scientific results show a high absolute accuracy. The present radar network has a data frequency of 6 pictures / hour, and a spatial resolution of 2 km x 2 km. Surface Radiation and Sunshine Observing Network Regarding observations of hours of bright sunshine DMI runs a network of 30 stations in Denmark, 6 in Greenland and one on the Faroe Islands. Radiation is measured at 23 stations in Denmark, of which 15 are operated by DMI and 8 by the Danish Institute of Agricultural Sciences (DIAS). The measurements of radiation are carried out as 10- minute mean values of global radiation at the DMI operated stations and as hourly mean values of global radiation at the stations operated by DIAS. Solar Ultraviolet Radiation and Stratospheric Ozone stations The Solar Ultraviolet (UV) radiation at different wavelenghts is measured by DMI at two sites in Greenland, namely Pittufik and Kangerlussuaq. Besides the GO3OS described earlier weekly ozone soundings are made at Illoqqortoormiut and sporadic ozone soundings are made during the winter months in Pituffik by DMI. Upper Air Measurements - Radiosounding Observations DMI runs radiosounding stations in the following 7 locations: Copenhagen (Denmark),Tórshavn (the Faroe Islands), Danmarkshavn, Illoqqortoormiit, Tasiilaq, Narsarsuaq and Aasiaat (Greenland). Two soundings are made every day at these stations. From all 7 radiosounding stations a monthly summary (CLIMAT TEMP) is prepared and transmitted routinely on the GTS. DMI has the responsibility of systematic surveillance of the sea ice conditions in the Greenland waters. Observations on the ice conditions have been collected for approximately 125 years and an extensive volume of data is available in a graphic format as monthly summaries, ice maps etc. Since 1959 special emphasis has been put on the waters south of Cape Farewell (the southern tip of Greenland) in order to improve the navigation safety. Ice maps are prepared more than weekly containing detailed information on the relevant ice conditions. Recent maps are available on vector graphic format. Since 2000 weekly summaries of the ice conditions for all Greenland waters have been prepared. These summaries are based on satellite data and are generated automatically and are primarily intended for analysis of the climatology in the Greenland waters. Over the years several long term climatological series have been established by DMI representing Denmark, Greenland and the Faroe Islands. The main accomplishments in this area in recent years are: - Observed Daily Precipitation,Temperature and Cloud Cover for Seven Danish Sites, 1874-2000 (DMI technical report no. 01-10) and Observed Daily Precipitation, Maximum Temperature and Minimum Temperature from Ilulissat and Tasiilaq, 1873-2000 (DMI technical report no. 01-11). Both reports (incl. datasets) are available at DMI's website (http://www.dmi.dk/eng/f+u/index.ht ml) under the headings Publications / Technical Reports. Automatic monitoring takes place near ground level in both urban and rural locations across Denmark. A monitoring network is operated by the National Environmental Research Institute (NERI), Denmark, and measures a wide range of pollutants:
Figure 6 shows the types and distribution of air quality monitoring stations across Denmark and in table 2 the measurements taken at the different stations are listed. Besides the above measured ozone DMI operates an ozone measurement station at Jægersborg a suburban environment near Copenhagen. Real-time hourly data are presented on DMI's website (http://www.dmi.dk). Data with a time resolution of 10 minutes are available from DMI. It is intended to establish one more real-time ozone measurement station in 2002.
Figure 6: Table 2:
Chapter 3 Oceanographic ObservationsFor the oceanographic observations GCOS is based upon the open ocean (climate) module of GOOS, which comprises the following programmes: drifting and moored buoy programmes managed by the DBCP (Data Buoy Co-operation Panel), the Ship of Opportunity Programme (SOOP), the Argo array of profiling floats, the Global Sea Level Observing System (GLOSS), the Voluntary Observing Ships Programme (VOS) and the Automated Shipboard Aerological Programme (ASAP). Denmark participates in the VOS, GLOSS and ASAP programmes as summarised in table 3 below. Table 3:
VOS is an international scheme, first developed almost 150 years ago, by which ships plying the various oceans and seas of the world are recruited for taking and transmitting meteorological observations.VOS ships make a highly important contribution to the Global Observing System (GOS) of the World Weather Watch (WWW), and increasingly, through the VOS Climate Project (VOSClim), to global climate studies.VOS is disseminated on the GTS and are archived by many national meteorological services. At the end of 2000 the Danish fleet of voluntary observing ships consisted of 47 ships. DMI has the operational and professional responsibility for the observations, which are made every third hour from the ships. GLOSS is an international programme coordinated by the IOC for the establishment of high quality global and regional sea level networks for application to climate, oceanographic, and coastal sea level research. The main component of GLOSS is the Global Core Network (GCN) of 287 sea level stations around the world for long-term climate change and oceanographic sea level monitoring. GLOSS stations are established in Torshavn (Faroe Islands), Nuuk (Greenland) and Ammassalik (Greenland). The former GLOSS stations in Ittoqqortoormiit and Danmarkshavn (both in Greenland) have been abolished. The station in Ammassalik is operated by the Royal Danish Administration for Navigation and Hydrography, whereas the other two stations are operated by DMI. The relevant mean values from the stations are transmitted to the Permanent Service for Mean Sea Level (PSMSL) hosted by the Proudman Oceanographic Laboratory in the UK. The PSMSL was established in 1933, and is the global data bank for long-term sea level change information from tide gauges. Information on monthly and annual mean sea level is transmitted to PMSLS from 15 stations in Denmark, 5 in Greenland and one on the Faroe Islands. Automated Shipboard Aerological Programme /ASAP The ASAP in its present form began in the mid-1980. It involves the generation of upper air profile data from data sparse ocean areas using automated sounding systems carried on board merchant ships plying regular ocean routes. Several National Meteorological Services operate ASAP units and the profile data are made available in real time on the GTS. ASAP data are archived alongside other radiosounding data by many national meteorological services. ASAP is an important contribution to both the WWW and GCOS. Most of the soundings are presently from the North Atlantic and NorthWest Pacific Oceans, but the programme is expanding to other ocean basins, through a new, co-operative Worldwide Recurring ASAP Project (WRAP). Denmark operates two ASAP units, mounted on ships plying routes from Denmark to Greenland. The European meteorological cooperation EUMETNET started a special E-ASAP programme December 2000. Currently two ASAP units are operated under this programme, one in the Mediterranean and one in the Atlantic. DMI is the responsible member for this programme. Other National Oceanographic and Marine Observations In Denmark a Network exists for the collection of sea temperatures at 13 coastal stations around Denmark. The stations are operated by DMI, the Royal Danish Administration for Navigation and Hydrograhy and local authorities respectively. Data are available from each of the responsible bodies. In Greenland a total of 7 stations measure sea temperatures. DMI and the Royal Danish Administration for Navigation and Hydrograhy operates the stations. In Denmark an extensive national network of tide gauges are operated jointly by DMI, the Royal Danish Administration for Navigation and Hydrograhy, local authorities and the Danish Coastal Authority. The network consists of 82 automatic stations. In Greenland a total of 7 tide gauge stations are operated by DMI and the Royal Danish Administration for Navigation and Hydrograhy. On the Faroe Islands one station is operated in Torshavn by DMI. Data are available from the responsible bodies. Hydrographic and Marine Surveys The National Environmental Research Institute has the overall responsibility for surveillance of the Danish Waters. Regular Surveys are carried out with the objectives of:
Surveys are part of the Danish nationwide monitoring programme NOVA 2003, the HELCOM monitoring programme for the Baltic Sea area (Arkona Sea, Sound, Belt Sea, Kattegat), and the OSPARCOM monitoring programme for the Greater North Sea (Kattegat, Skagerrak, North Sea). The Danish Institute for Fisheries Research carries out yearly surveys in the Danish Waters, primarily in the North Sea and the Baltic Sea, and in that relevant oceanographic parameters are measured and recorded. Furthermore, DMI is involved in the following projects: Biogeochemical cycling of Carbon and Ocean circulation in the northern North Atlantic The overall aim of the project is to describe the effect of high latitude carbon dynamics on the global ocean atmosphere carbon system, in general, and on atmospheric pCO2 in particular. At present, knowledge concerning the seasonal differences in turnover rates of organic material in Polar and sub-polar regions is limited. Thus, in order to achieve the aim of this project it is necessary to obtain biological and chemical rate measurements for the production and destruction of dissolved and particulate organic material at high latitudes and relate these to the convection occurring at different times of the year. Measurements of water transports across the Greenland-Scotland Ridge During the Nordic WOCE programme (1993-97) observations of the water transport across the Greenland Scotland Ridge was initiated and the measurements have been continued after the closing of the Nordic WOCE programme. The goal of the observation campaign was to put reliable numbers on the volume transports of the various current components flowing in and out of the Nordic Seas, and especially to investigate possible seasonal and interannual variability, which might reflect changes in the global thermohaline circulation. Monitoring of the oceanographic conditions along West Greenland Denmark/Greenland has in relation to the North Atlantic Fisheries Organisation (NAFO) the responsibility for monitoring the physical oceanographic conditions along the westcoast of Greenland. The formal responsibility for performing these measurements is placed at the Greenland Institute for Natural Resources, Nuuk which since 1998 has allocated the work by contract to the Danish Meteorological Institute.
Figure 7: The temperature and salinity is measured on standard stations along the Greenland westcoast with the purpose of obtaining knowledge about the marine climate in the area which has a great impact on the recruitment and survival of the fish species living in the area of which some is living close the limit of survival. The data therefore are of great importance to the fisheries' assessment work. Monitoring of the oceanographic conditions around the Faroe Islands. The Fisheries Laboratory in Thorshavn monitors the oceanographic conditions around the Faroe Islands on four standard sections four times a year. The purpose of the monitoring is to study the water mass composition and its variability in the area. Chapter 4 Terrestrial ObservationsExcept monitoring of snow cover, sea ice and surface radiation Denmark does not carry out further terrestrial observations that can be related to climate change. However, Denmark's climate related research includes monitoring and studying the effect of terrestrial conditions. Chapter 5 Space-based ObservingDenmark contributes to space based observations through the European agencies ESA (a partnership of 15 European Member Governments, with Canada affiliated), EUMETSAT (a partnership of 17 European Member Governments, with three Cooperating States) and by the utilisation of national small satellites. As such, details of the platforms and sensors are not given in this section, which focuses on Danish specific needs and efforts. The Danish strategy for earth observations (EO) is delivered, largely, through participation in international programmes and to some extent through national programmes such as the Ørsted satellite. The Danish space activities are not coordinated by one central institution. The Ministry for Science,Technology and Innovation represents Denmark in ESA, whereas the responsibility for the meteorological observation aspects (EUMETSAT) lies with the Ministry of Transport. The actual activities are carried out by several organisations, such as DMI, the Technical University of Denmark, Danish Space Research Institute and of course private industry. ESA and EUMETSAT Platforms and Programmes ESA EO platforms that are either operational now or due for launch before the end of 2005 and the projects where Denmark is participating, include:
It can further be mentioned that Denmark has been involved in the preparation for new programmes under the ESA-EO:WATS as a core mission and ACE+ as an opportunity mission. The purpose of these missions is to obtain reliable data on the temperature, pressure and humidity of the atmosphere amongst others to secure a better understanding of climate variations. DMI represents Denmark in EUMETSAT, which has the following current programmes:
As part of its distributed application ground segment EUMETSAT has a network of Satellite Application Facilities (SAFs), as specialised development and processing centres (see http://www.eumetsat.de for details). These utilise the specific expertise available in EUMETSAT's Member States, and complement the production of standard meteorological products derived from satellite data at EUMETSAT's Central Facilities in Darmstadt. Seven SAF projects are undergoing development, focusing on the following applications:
A number of these are relevant to aspects of GCOS monitoring. DMI hosts the GRAS meteorology SAF and also contributes the Ocean and sea ice SAF and the Ozone monitoring SAF. GPS data from the Ørsted, SACC and CHAMP satellites Measurements of GPS radio occultations are important in use both for numerical weather prediction and to monitoring of climate change processes and their identification. This has been demonstrated first by the American proof-of-concept mission GPS/MET. The research satellites Ørsted, SAC-C and CHAMP all have the capability of the required high precision reception of GPS signals to perform radio occultation measurements. The GPS data from the Danish Ørsted satellite, launched in 1999, has been used in the EU project CLIMAP (CLImate and environment Monitoring with GPS based Atmospheric Profiling) to study the impact on numerical weather prediction. Further, since the data needs no calibration, they will prove very valuable for climate monitoring purposes by combining several data sets and model forecasts. The primary objective of the CLIMAP project was to establish endtoend demonstrations of the operational derivation and usage in Numerical Weather Prediction (NWP) of atmospheric parameters on basis of the reception of GPS signals through the atmosphere. This included data from GPS reception on ground and Radio Occultations from Low Earth Orbiting (LEO) satellite based GPS reception. An "end-to-end" chain for processing of satellite based GPS radio occultation data was developed: From GPS signal reception to assimilation into the NWP models. The chain included operational reception of tracking data from the Ørsted satellite with associated level 0 processing and archiving (operational and prepared by the Danish company TERMA and DMI). This Ørsted processing chain will be further used by DMI on the new GPS occultation data received by the German CHAMP and the Argentinean SACC satellite. Chapter 6 Activities in Developing Countries relating to Observations.DMI has since 1997 participated in a project at the Meteorological Services Department of Ghana (MSD). The aim of the project is primarily to re-establish the meteorological observing network in the country and ensure the collection of data. Another part of the project is the communication and utilisation of the data. The Project will continue to the end of 2003, and by that time MSD should operate a well-functioning network of approximately 300 stations recording the basic meteorological parameters. The project is funded by the Danish State aid organisation DANIDA. List of Acronyms
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