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Based on common template, EEA has analysed the Copernicus Land Monitoring Service Corine Land cover data for 2000-2018. The set of interactive dashboards provide graphs and maps with concise characterization of land cover changes in the EEA38 member and collaborating countries.
Extreme sea levels have increased at most locations along the European coastline. Both observed and projected increases can be explained mainly by increases in mean local sea levels. However, extreme sea levels can be further increased by storm surges and tidal changes, particularly along the northern European coastline. In the absence of better coastal protection, the sea level rise projected for 2100 will increase the frequency of extreme coastal flooding events by a factor of 10 to more than 1 000 along most European coastlines, depending on the location and the emissions scenario.
Ecosystem Extent Accounts are derived from the Copernicus Land Monitoring Service Corine Land Cover datasets every six years from 2000 till 2018. They describe the extent of various ecosystem types in the EEA38+UK region and how they change over time.
The map show the trade flow of primary plastics between EU-28 and the most important trade partners for each category. Arrows outbound from EU-28 shows exported value and inbound show imported value.
The dataset consists of a collection of annual soil moisture (SM) anomalies during the vegetation growing season (GS) for the years 2000-2019 across EEA 38 area and the United Kingdom. The vegetation growing season is defined by EEA´s phenology data series "Vegetation growing season length 2000-2016" [https://www.eea.europa.eu/data-and-maps/data/annual-above-ground-vegetation-season]. The anomalies are calculated based on the European Commission's Joint Research Centre European Drought Observatory (EDO) Soil Moisture Index (SMI) with respect to the 1995–2019 base period. The yearly start and end of GS periods are dynamic and calculated according to the EEA Phenology Indicators. A positive anomaly indicates that the observed SM was wetter than the long-term SM average for the base period, while a negative anomaly indicates that the observed SM was drier than the reference value. Because SM anomalies are measured in units of standard deviation from the long-term SMI average, they can be used to compare annual deficits/surplus of SM between geographic regions. EDO is one of the early warning and monitoring systems of the Copernicus Emergency Management Service. As the dataset builds on EDO's SMI, it therefore contains modified Copernicus Emergency Management Service information (2019).
This dashboard presents country profiles containing key data on greenhouse gas (GHG) emissions, renewable energy and energy efficiency for each EU Member State. These country profiles support and complement the assessment of progress towards climate and energy targets in Europe.
Between 1980 and 2019, climate-related extremes caused economic losses totalling an estimated EUR 446 billion in the EEA member countries. Although analysing trends in economic losses is difficult, partly as a result of high variability from year to year, climate-related extremes are becoming more common and, without mitigating action, could result in even greater losses in the coming years. The EU adaptation strategy aims to build resilience and ensure that Europe is well prepared to manage the risks and adapt to the impacts of climate change, thus minimising economic losses and other harms.
The ozone hole is a region of exceptionally depleted ozone in the stratosphere over the Antarctic. All figures are in million square kilometres.
The area and number of terrestrial protected areas in Europe have grown steadily over time, with the biggest increases in recent decades. In 2020, protected areas covered 26 % of EU land, with 18 % designated as Natura 2000 sites and 8 % as other national designations. In the EEA-38 countries plus the United Kingdom, this coverage is lower and amounts to 23 %. Further expansion of terrestrial protected areas will be needed to achieve the target of legally protecting a minimum of 30 % of EU land, as set out in the EU biodiversity strategy for 2030. The designation of protected areas is not in itself a guarantee of biodiversity conservation. Effective management requires building a coherent and well-connected network of protected areas with clearly defined conservation objectives and measures.
At the EU level, only 15 % of habitat assessments have a good conservation status, with 81 % having poor or bad conservation status. Grasslands, dunes, and bog, mire and fen habitats show strong deteriorating trends, while forests have the most improving trends. The EU is not on track to meet the 2020 target of improving the conservation status of EU protected species and habitats. At the EU Member State level, the majority of assessments indicate a low number of habitats with a good conservation status. Intensive agriculture, urban sprawl and pollution are the top reported pressures to habitats.
After increasing for 13 years, fluorinated greenhouse gas (F-gas) emissions in the EU decreased for the first time in 2015, and fell by 5 % in 2018 compared to 2017. This can be partly attributed to the EU-wide hydrofluorocarbon (HFC) phase-down set out in the F-gas Regulation, which aims to reduce F-gas emissions and mitigate global warming. HFCs account for the majority of F-gas emissions and the EU is on track to meet targets and phase down HFC use by 2030. It is also on track to meet its international obligation to reduce HFC consumption, in effect since 2019, under the Montreal Protocol.
Impacts of extreme weather and climate related events in the EEA member countries.
Impacts of extreme weather and climate related events in the EEA member countries.
Impacts of extreme weather and climate related events in the EEA member countries and the UK.
Impacts of extreme weather and climate related events in the EEA member countries and the UK
Global mean sea level (GMSL) has risen about 19 cm since 1900, at an accelerating rate. GMSL reached its highest value ever in 2019. Climate models project a GMSL rise during the 21st century that will likely be in the range of 0.29-0.59 m for a low emissions scenario and 0.61-1.10 m for a high one. GMSL projections that include the possibility of faster disintegration of the polar ice sheets predict a rise of up to 2.4 m in 2100 and up to 15 m in 2300. Most coastal regions in Europe have experienced an increase in sea level relative to land, except for the northern Baltic coast.
For references, please go to https://www.eea.europa.eu/data-and-maps/find/global or scan the QR code.
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Software updated on 26 September 2023 08:13 from version 23.8.18
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