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Greenhouse gas emissions from land use, land use change and forestry

Through its land use, land use change and forestry (LULUCF) activities, the EU currently removes a net total of 249 Mt CO 2 e from the atmosphere every year, equivalent to 7% of its annual greenhouse gas emissions. The sector will play a crucial role in helping the EU achieve net zero emissions by 2050. Doing so will require reversing the current decreasing trend of the EU's  carbon sink . According to national projections from EU Member States, current measures in place will not be sufficient to achieve this, with an average removal of 200 Mt CO 2 e per year in 2030. However, implementing the national measures currently at planning stage could increase the current EU carbon sink by 3%.

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Soil moisture deficit

Soil moisture deficit

22 Mar 2021

Monitoring the pressure from soil moisture deficits can warn of potential impacts on plant development and soil health, supporting the assessment of drought-tolerant, resilient and vulnerable ecosystems. In 2000-2019, soil moisture in the growing season was several times below the long-term average in the EEA member countries plus the United Kingdom. The largest soil moisture deficits occurred in 2003, 2017 and 2019, affecting over 1.45 million km 2 in 2019. Soil moisture content was also low in 2012, 2015 and 2018, contributing to increasingly frequent and intense drought pressure.

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Drought impact on ecosystems in Europe

Monitoring  vegetation response to water deficit due to droughts is necessary to be able to introduce effective measures to increase the resilience of ecosystems in line with the EU’s nature restoration plan — a key element of the EU biodiversity strategy for 2030. Between 2000 and 2016, Europe was affected by severe droughts, causing average yearly vegetation productivity losses covering around 121 000 km 2 . This was particularly notable in 2003, when drought affected most parts of Europe, covering an estimated 330 000 km 2  of forests, non-irrigated arable land and pastures. Drought impact was also relatively severe in 2005 and 2012.

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Imperviousness and imperviousness change in Europe

For the reference year 2015 ,  85 861 km 2   of the total area covered by the  EEA-39 countries were mapped and categorised as 'sealed surface' in the Copernicus imperviousness product. This corresponds to 1.466 % of the total EEA-39 area. Between 2006 and 2015, soil sealing (imperviousness) in all EEA-39 countries increased  by a total of 3 859 km2 , an annual average increase of 429 km 2 . During this period, the average annual increase in soil sealing relative to country area varied from 0 % to 0.088 %. In 2015, the percentage of a countries' total area that was sealed also varied greatly, with values ranging from 16.17 % (Malta) to 0.07 % (Iceland). The highest sealing values, as a percentage of country area, occurred in small countries with high population densities, while the lowest sealing values can be found in large countries with low population densities. The average annual increase in sealing was 460 km 2 between 2006-2009, increasing to 492 km 2 for the 2009-2012 period and slowing to 334 km 2 for the 2012-2015 period. The slow-down in the sealing increase between the two reference  periods occurred in 31 out of 39 countries. The same trend is visible for sealing figures normalised by the size of the country (the % of the country newly sealed on average annually for the three periods). The most problematic situation occurs in countries where there is already a high percentage of sealing and where the annual rate of increase relative to country area is high. Even more problematic are situations where, for 2012-2015,  the rate of sealing increase is accelerating, in contrast to the general trend of a slowing rate of increase.  

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Vegetation productivity

Vegetation productivity indicates the spatial distribution and change of the vegetation cover - a key characteristic of ecosystem condition.  Vegetation productivity in Europe on average has a regional pattern of increase and decline. Increase was observed most in South Eastern Europe, over croplands and wetlands in the Steppic region and grasslands and sparsely vegetated lands and in the Black Sea and Anatolian regions. Decline happened most over croplands and grasslands in the Atlantic region as well as over wetlands in the Alpine region. Climate has important influence on vegetation productivity in Europe. Strongest driver is precipitation, especially in the South Eastern regions. Decreasing number of frost days increased productivity in the Pannonian region but decreased productivity in the Atlantic region. Climatic variations are important drivers of vegetation productivity, but land use changes are even stronger. Productivity was most increased by agricultural land management and converting other lands to agriculture, whereas largest decrease was caused by sprawling urban areas.

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Landscape fragmentation pressure and trends in Europe

In 2015, on average, there were around 1.5 fragmented landscape elements per km 2 in the European Union  [1] , a 3.7 % increase compared with 2009. Approximately 1.13 million km 2 , around 28 % of the area of the EU  [1] , was strongly fragmented i n 2015 , a 0.7 % increase compared with 2009. There was less of an increase in fragmented landscape elements and in the area of strongly fragmented landscape between 2012 and 2015 than between 2009 and 2012 (1.4 and 0.18 percentage points, respectively). Arable lands and permanent croplands (around 42 .6 %) and pastures and farmland mosaics (around 40.2 %) were most affected by strong fragmentation pressure in 2015 in the EU. Between 2009 and 2015, however, the largest increase in the area of strongly fragmented landscape was in grasslands/pastures and in farmland mosaics.   Luxembourg (91 %), Belgium (83 %) and Malta (70 %) had the largest proportions of strongly fragmented landscape in 2015 (as a proportion of their country area). The Baltic countries and Finland and Sweden were on average the least fragmented countries in the EU. Between 2009 and 2015, the area of strongly fragmented landscape increased most in Croatia, as well as in Greece, Hungary and Poland. [1]  Romania is excluded because of the poor coverage of fragmentation geometry data in 2009.  

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Land recycling and densification

Land recycling is still low in all European countries: on average, land recycling accounted for only 13.5 % of total land consumption in European cities in the 2006-2012 period. The land use densification process, i.e. when land development makes maximum use of existing infrastructure, accounts for the largest proportion of land recycling. However, in most countries, land take dominates over densification in total land management with the exception of Finland and France. Grey recycling, i.e. internal conversions between residential and/or non-residential land cover types, is secondary to densification, ranging from 14 % to less than 1 % of total land consumption. Land take predominates over grey recycling in total land management in all countries. Green recycling, i.e. the development of green urban areas using previously built-up areas, is an important trend that reverses soil sealing, but it is a marginal process in all countries and, on average, it accounts for only 0.2 % of total land consumption.

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