State

Southern half of Norway still suffering from damage

Deposition of sulfur and nitrogen can lead to acidification of water and soil. In Norway acidification, results in reduced water quality in lakes and rivers in the southern half of Norway, and especially in the southernmost counties. Over the years many fish stocks have been depleted or wiped out, and other aquatic animals and plants are also affected.

pH trends in lakes from 1990 to 2013

Sulphur causes acidification in Norway

Deposition of sulphur causes acidification in Norway, and sulphur deposition is highest in the most sensitive areas in the south. As sulphur emissions are being reduced more rapidly than nitrogen emissions, the relative importance of nitrogen as a source of pollution is increasing.

Nitrogen also has other effects

Nitrogen has more complex ecological effects than sulphur, because it can also act as a fertiliser and cause eutrophication. Most nitrogen is absorbed by plants or the soil, but the remainder ends up in fjords and coastal waters, where it can fuel eutrophication and excessive algal growth.

Critical loads low in the southern half of Norway

Critical loads are used to define the amount of pollution different ecosystems can absorb without damage to the natural environment. In Norway, freshwater ecosystems are particularly sensitive to acidification. Critical loads for freshwater are based on the effects on trout. They are particularly low in the southern half of the country, mainly because soils are thin and the bedrock consists of acidic rocks such as gneiss and granite.

Impact

Acid rain kills fish

Salmon stocks lost in the southernmost counties

Acid rain is still a serious threat to biodiversity in rivers and lakes in Norway. In all, more than 9000 fish stocks were lost and over 5000 were severely depleted due to acidification in 1990. Similar calculations have not been performed since, but in a study from 2008, it was estimated that the area with damage to fish stocks in Norway was reduced from around 20 000 km2 in 1990 to 13 000 km2 in 2006, a reduction of about 38 percent.

Little or no damage to Norwegian forests

In the 1980s, acid rain resulted in widespread damage to forests in the border areas between Poland and the former East Germany and Czechoslovakia. There was serious concern about similar damage in Norway, and in 1984 the Norwegian Monitoring Programme for Forest Damage was started.

On the whole, Norwegian forests appear to have tolerated sulphur and nitrogen deposition without serious effects. They showed a decrease in vitality (measured as crown density) during the 1990s, but since then conditions have improved. In the last few years, the health of Norwegian forests has remained stable.

Major economic consequences

In addition to its effects on ecosystems, acid rain has serious consequences for society as a whole. One example is that loss of fishing opportunities can lead to economic losses for businesses in the affected areas. About 78-88 million NOK has therefore been spent annually on liming of rivers and lakes in recent years. Acidification may also damage buildings, sculptures, rock art and other parts of our cultural heritage. 

Driving forces

Trends determined by energy use

Acid rain is mainly caused by combustion of fossil fuels. More than 90 per cent of the sulphur and 80 per cent of the nitrogen deposited in Norway originates in other European countries. The UK, Germany, Poland and the North Sea are among the most important sources. This means that the amount of acid rain falling on Norway is to a large extent determined by developments elsewhere in Europe.

The European emissions have been greatly reduced over the last 20-30 years. This is largely due to technical improvements in industrial processes, and a transition from coal to fuels with less sulphur. There has not been a corresponding reduction in the emissions of nitrogen, because these emissions are highly influenced by the use of transport. 

Pressure

Industry and transport the main sources

Power plants, industrial processes (especially metal production) and transport are the main sources of acidifying emissions.

Sulphur and nitrogen deposition in Norway declining

Inputs of sulphur and nitrogen to Norway have declined as emissions in Europe have been reduced. However, there has been a much smaller overall reduction for nitrogen (sum of oxidised and reduced nitrogen) than for sulphur. There are several reasons for this:

  • it took much longer before people began to focus on the harmful effects of nitrogen 
  • it took longer before international agreements on the reduction of nitrogen emissions were concluded
  • the mix of sources is different for nitrogen, and this has made it more difficult to find effective ways of reducing emissions.
Read more about the data | Share graf

 

Total deposition of sulphur in Norway was reduced from about 200 000 tonnes in 1980 to 34 000 tonnes in 2010, a reduction of more than 80 per cent.

Total deposition of nitrogen in Norway was about 100 000 tonnes in 1980, and increased to 130 000 in 1990. From 1990 to 2010 deposition was almost halved, from 130 000 tonnes to 66 000 tonnes.

Norwegian sulphur and nitrogen emissions declining

In Norway, the main sources of sulphur dioxide emissions are metal production, stationary combustion and other industrial processes. Norwegian emissions have been greatly reduced, from about 150 000 tonnes a year in the 1970s to about 17 000 tonnes in 2013.

The main sources of nitrogen emissions in Norway are coastal shipping, fishing vessels, the oil and gas industry and road traffic. In 2013, emissions were about 162 000 tonnes. In addition, there was a total emission of 27 000 tonnes of the nitrogen compound ammonia.

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Response

International agreements are vital

Acid rain does not respect national borders, and is a problem for most European countries. The answer has been to join forces to reduce overall European emissions of sulphur and nitrogen.

Binding international agreements

Most European countries have undertaken to reduce their emissions of acidifying substances through the Convention on Long-range Transboundary Air Pollution (LRTAP). Several binding protocols have been adopted under the convention, including the Gothenburg Protocol, which entered into force in 2005. Initially emissions ceilings were set for 2010, but the protocol was renegotiated in 2012 and new emissions ceilings (to be met in 2020) have been set.

Norway met the 2010 emission ceiling for sulphur dioxide in 2006, while emission ceilings for ammonia and nitrogen oxides were not met. The emissions of ammonia were about 4000 tonnes above the target of 23 000 tonnes in 2010. For nitrogen oxides the emission ceiling was 156 000 tonnes in 2010, while the Norwegian emissions were about 182 000 tonnes.

In the revised Gothenburg Protocol, Norway has undertaken to reduce emissions of sulphur dioxide, ammonia and nitrogen, by respectively 10, 8 and 23 per cent relative to emissions in 2005. For Norway, the new requirements represent only minor changes. For sulphur dioxide, the target was reached already in 2007. Emissions of ammonia must be reduced from 27 000 tonnes in 2013 to 25 000 tonnes in 2020, while emissions of nitrogen oxides must be reduced from 162 000 tonnes in 2013 to 156 000 tonnes in 2020. 

Liming reduces damage

Liming of rivers and lakes is an important means of remedying the worst of the damage caused by acid rain. The aim is to give animals and plants a chance to re-establish themselves. Each year 30 000 - 50 000 tonnes are applied in Norwegian rivers and lakes. The liming programme is most extensive in Telemark, Aust-Agder, Vest-Agder and Rogaland counties.