Coastal zones are presented as a series of 10 consecutive buffers of 1km width each (towards inland). For this dataset, were treated as sea data all areas with class values of 52x (521: coastal lagoons, 522: estuaries, 523: sea and ocean) in Corine Land Cover (details in lineage).

Coastal zones are presented as a series of 10 consecutive buffers of 1km width each (towards inland). For this dataset, were treated as sea data all areas with a class value of 523 (sea and ocean) in Corine Land Cover (details in lineage).

Coastal zones are presented as a series of 10 consecutive buffers of 1km width each (towards inland). For this dataset, were treated as sea data all areas with a class value of 523 (sea and ocean) in Corine Land Cover (details in lineage).

Coastal zones are presented as a series of 10 consecutive buffers of 1km width each (towards inland). For this dataset, were treated as sea data all areas with class values of 52x (521: coastal lagoons, 522: estuaries, 523: sea and ocean) in Corine Land Cover (details in lineage).

Complete Coastline Features for all the countries that produced Corine Land Cover 2000 and have a coastline, with detailed descriptions on the environment and type of coastal areas. Each coast segment has inherited CLC 2000 class, and also the attributes from Eurosion Coastline version 2.1 2004, regarding geomorphology, type of coast and erosion trends.

This dataset is the coastal zone land surface region from Europe, derived from the coastline towards inland, as a series of 10 consecutive buffers of 1km width each. The coastline is defined by the extent of the Corine Land Cover 2018 (raster 100m) version 20 accounting layer. In this version all Corine Land Cover pixels with a value of 523, corresponding to sea and oceans, were considered as non-land surface and thus were excluded from the buffer zone.

The Coastal Zones LC/LU Change (CZC) 2012-2018 is providing the Land Cover / Land Use (LC/ LU) change for areas along the coastline of the EEA38 countries and the United Kingdom, between the reference years 2012 and 2018. The Coastal Zones product monitors landscape dynamics in European coastal territory to an inland depth of 10 km with a total area of approximately 730,000 km², with all the relevant areas (estuaries, coastal lowlands, nature reserves). The production of the coastal zone layers was coordinated by the European Environment Agency (EEA) in the frame of the EU Copernicus programme, as part of the Copernicus Land Monitoring Service (CLMS) Local Component. The Coastal Zones Change product covers a buffer zone of coastline derived from EU-Hydro v1.1. The Land Cover/Land Use (LC/LU) Change layer is extracted from Very High Resolution (VHR) satellite data and other available data. The reference years for the change are 2012 and 2018. The class definitions follow the pre-defined nomenclature on the basis of Mapping and Assessment of Ecosystems and their Services (MAES) typology of ecosystems (Level 1 to Level 4) and CORINE Land Cover adapted to the specific characteristics of coastal zones. The classification provides 71 distinct thematic classes with a Minimum Mapping Unit (MMU) of 0.5 ha and a Minimum Mapping Width (MMW) of 10 m. The status product is available for the 2012 and 2018 reference years. This CZC dataset is distributed in vector format, in a single OGC GeoPackage file covering the area of interest. You can read more about the product here: https://land.copernicus.eu/en/products/coastal-zones/coastal-zones-change-2012-2018.

The Coastal Zones (CZ) LC/LU product for 2018 is providing a detailed Land Cover / Land Use (LC/ LU) dataset for areas along the coastline of the EEA38 countries and the United Kingdom, with reference year 2018 for the classification. This product monitors landscape dynamics in European coastal territory to an inland depth of 10 km with a total area of approximately 730,000 km², with all the relevant areas (estuaries, coastal lowlands, nature reserves). The production of the coastal zone layers was coordinated by the European Environment Agency (EEA) in the frame of the EU Copernicus programme, as part of the Copernicus Land Monitoring Service (CLMS) Local Component. The Coastal Zones product covers a buffer zone of coastline derived from EU-Hydro v1.1. Land Cover/Land Use (LC/LU) layer is extracted from Very High Resolution (VHR) satellite data and other available data. The class definitions follow the pre-defined nomenclature on the basis of Mapping and Assessment of Ecosystems and their Services (MAES) typology of ecosystems (Level 1 to Level 4) and CORINE Land Cover adapted to the specific characteristics of coastal zones. The classification provides 71 distinct thematic classes with a Minimum Mapping Unit (MMU) of 0.5 ha and a Minimum Mapping Width (MMW) of 10 m. The product is available for the 2012 and 2018 reference year including change mapping. This CZ dataset is distributed in vector format, in a single OGC GeoPackage SQLite file covering the area of interest. You can read more about the product here: https://land.copernicus.eu/en/products/coastal-zones/coastal-zones-2018.

The Coastal Zones (CZ) LC/LU product for 2012 is providing a detailed Land Cover / Land Use (LC/ LU) dataset for areas along the coastline of the EEA38 countries and the United Kingdom, with reference year 2012 for the classification. This product monitors landscape dynamics in European coastal territory to an inland depth of 10 km with a total area of approximately 730,000 km², with all the relevant areas (estuaries, coastal lowlands, nature reserves). The production of the coastal zone layers was coordinated by the European Environment Agency (EEA) in the frame of the EU Copernicus programme, as part of the Copernicus Land Monitoring Service (CLMS) Local Component. The Coastal Zones product covers a buffer zone of coastline derived from EU-Hydro v1.1. Land Cover/Land Use (LC/LU) layer is extracted from Very High Resolution (VHR) satellite data and other available data. The class definitions follow the pre-defined nomenclature on the basis of Mapping and Assessment of Ecosystems and their Services (MAES) typology of ecosystems (Level 1 to Level 4) and CORINE Land Cover adapted to the specific characteristics of coastal zones. The classification provides 71 distinct thematic classes with a Minimum Mapping Unit (MMU) of 0.5 ha and a Minimum Mapping Width (MMW) of 10 m. The product is available for the 2012 and 2018 reference year including change mapping. This CZ dataset is distributed in vector format, in a single OGC GeoPackage SQLite file covering the area of interest. You can read more about the product here: https://land.copernicus.eu/en/products/coastal-zones/coastal-zones-2012.

Les variations barystatiques et manométriques du niveau marin représentent la composante de masse des variations du niveau marin aux échelles globale et régionale respectivement. Les variations barystatiques et manométriques du niveau marin sont estimées ici à partir de la gravimétrie, issues des mesures des missions de gravimétrie spatiale GRACE et GRACE - Follow On. Deux produits sont distribués sur la période avril 2002 à août 2022 : - Les variations barystatiques du niveau de la mer à partir de la gravimétrie : séries temporelles mensuelles, - Les variations manométriques du niveau de la mer à partir de la gravimétrie : grilles mensuelles 1x1°. Les variations BARYSTATIQUES du niveau marin représentent les échanges de masses d’eau des continents aux océans et vice versa. La fonte des calottes polaires et des glaciers continentaux constituent les principales sources de variation du niveau barystatique. A l'échelle interannuelle, les échanges d'eau douce avec les grands bassins hydrologiques (par exemple l'Amazone, Mississippi) sont également importants. Les changements MANOMETRIQUES du niveau de la mer sont dus à plusieurs processus, incluant la circulation océanique et atmosphériques, les empreintes du niveau de la mer (sea level fingerprints en anglais) ou le cycle global de l'eau. Les modes climatiques, tels que l'oscillation australe d'El Niño, l'oscillation arctique, l'oscillation nord-atlantique ou le mode annulaire austral, influencent également de manière significative les changements manométriques du niveau de la mer Pfeffer et al., 2022). Les missions GRACE et GRACE Follow-On surveillent les variations temporelles du champ de gravité de façon quasi continue depuis 2002. De nombreux centres distribuent des solutions temporelles du potentiel gravitationnel de la Terre, fournies sous forme de coefficients de Stokes, connues sous le nom de solutions de niveau-2. Les solutions de niveau-2 doivent être corrigées de plusieurs effets géophysiques et erreurs instrumentales, converties en anomalies de masse de surface et projetées sur l'ellipsoïde. Les grilles d'anomalies de masse de surface qui en résultent, après application des corrections appropriées, sont appelées solutions de niveau-3. Plusieurs sources d'erreurs affectent les solutions des niveaux 2 et 3, imposées par la configuration du satellite, les erreurs instrumentales et les incertitudes dans les corrections géophysiques utilisées pour traiter les mesures. L'approche d'ensemble de Blazquez et al. (2018) est utilisée pour estimer de manière robuste les changements manométriques et barystatiques du niveau de la mer et leurs incertitudes. Références bibliographique - Blazquez, A., Meyssignac, B., Lemoine, J.-M., Berthier, E., Ribes, A., Cazenave, A. (2018). Exploring the uncertainty in GRACE estimates of the mass redistributions at the Earth surface: implications for the global water and sea level budgets, Geophysical Journal International, 215 (1), 415–430, https://doi.org/10.1093/gji/ggy293 - Pfeffer, J., Cazenave, A. & Barnoud, A. (2022). Analysis of the interannual variability in satellite gravity solutions: detection of climate modes fingerprints in water mass displacements across continents and oceans. Clim Dyn 58, 1065–1084. https://doi.org/10.1007/s00382-021-05953-z