Data centre overview

The European inventory of nationally designated protected areas holds information about designated areas and their designation types, which directly or indirectly create protected areas. This is version 20 and covers data reported until May 2022.

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These excel data files contains the result of a quickscan of literature regarding information on carbon stocks and carbon sequestration rates in terrestrial and marine ecosystems. Based on this information, supplemented with expert knowledge, a list has been drawn up in which the EUNIS habitat types are classified based on their total carbon stock and carbon sequestration rate. This list is available as separate excel worksheet for marine and terrestrial ecosystems and also included as annex in the report that documents the project.

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Landscape fragmentation is the physical disintegration of continuous ecosystems into smaller units, which is most often caused by urban or transport network expansion. Breaking structural connections between habitats results in decreased resilience of habitats and a decrease in their ability to provide various ecosystem services and support biodiversity. This dashboard enables the exploration of landscape fragmentation in Functional Urban Areas (FUAs) in Europe for the year 2018.

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Land take and the associated soil sealing causes less resilient ecosystems through landscape fragmentation and habitats destruction, soil sealing, decreased carbon sequestration and impaired flood protection. These processes are one of the major drivers of land degradation. Restoring wetlands, peatlands, coastal ecosystems, forests, grasslands and agricultural soils are essential for avoiding biodiversity decline and for climate change adaptation. This dashboard presents an overview of land take processes in floodplains of Functional Urban Areas in EEA and EU member states for the years 2012-2018. The amount of land take was derived from the Urban Atlas datasets of the Copernicus Land Monitoring Service.

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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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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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The map shows the long-term impact of water deficit on vegetation productivity, and the area of low vegetation productivity under water deficit impact, aggregated by NUTS3 regions. Negative anomalies are expressed in standard deviation and indicate vegetation productivity conditions that are lower than the long-term average under normal, non-drought conditions.

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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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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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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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Landscape fragmentation is the physical disintegration of continuous ecosystems into smaller units, which is most often caused by urban or transport network expansion. Breaking structural connections between habitats results in decreased resilience of habitats and a decrease in their ability to provide various ecosystem services and support biodiversity. This dashboard enables the exploration of landscape fragmentation in Functional Urban Areas (FUAs) in Europe for the year 2018.

Read more

Land take and the associated soil sealing causes less resilient ecosystems through landscape fragmentation and habitats destruction, soil sealing, decreased carbon sequestration and impaired flood protection. These processes are one of the major drivers of land degradation. Restoring wetlands, peatlands, coastal ecosystems, forests, grasslands and agricultural soils are essential for avoiding biodiversity decline and for climate change adaptation. This dashboard presents an overview of land take processes in floodplains of Functional Urban Areas in EEA and EU member states for the years 2012-2018. The amount of land take was derived from the Urban Atlas datasets of the Copernicus Land Monitoring Service.

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Land take and the associated soil sealing causes less resilient ecosystems through landscape fragmentation and habitats destruction, soil sealing, decreased carbon sequestration and impaired flood protection. These processes are one of the major drivers of land degradation. Restoring wetlands, peatlands, coastal ecosystems, forests, grasslands and agricultural soils are essential for avoiding biodiversity decline and for climate change adaptation. This dashboard presents an overview of land take processes in protected areas of Functional Urban Areas in EEA and EU member states for the years 2012-2018. The amount of land take was derived from the Urban Atlas datasets of the Copernicus Land Monitoring Service.

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The map shows the long-term impact of water deficit on vegetation productivity, and the area of low vegetation productivity under water deficit impact, aggregated by NUTS3 regions. Negative anomalies are expressed in standard deviation and indicate vegetation productivity conditions that are lower than the long-term average under normal, non-drought conditions.

Read more