Additional Products
Copernicus European Digital Elevation Model (EU-DEM), version 1.1 in 25m resolution
The EU-DEM v1.1 is a resulting dataset of the EU-DEM v1.0 upgrade which enhances the correction of geo-positioning issues, reducing the number of artefacts, improving the vertical accuracy of EU-DEM using ICESat as reference and ensuring consistency with EU-Hydro public beta.EU-DEM v1.1 is available in Geotiff 32 bits format. It is a contiguous dataset divided into 1000 x 1000 km tiles, at 25m resolution with vertical accuracy: +/- 7 meters RMSE. The tiles have been grouped in big regions:EUDEM2_ASIA (Turkey); EUDEM2_ATLAN (Hondo and Fr_Islands);EUDEM2_BRITAIN (Thames, Shannon and Tweed); EUDEM2_EUROPE_1 (Duero, Ebro, Tajo, Guadalquivir and Jucar); EUDEM2_EUROPE_2 (Tirso, Mesima, Tevere and Po); EUDEM2_EUROPE_3 (Garonne, Rhone, Loire, Seine and western Rhine); EUDEM2_EUROPE_4 (Danube); EUDEM2_EUROPE_5 (Skjern, Nemunas, Vistula, Oder, Elbe and Eastern Rhine); EUDEM2_EUROPE_6 (Bulgaria and Pinios); EUDEM2_ICELAND (Iceland); EUDEM2_SCAND (Vorma, Gota, Angerman, Tana, Kemi and Neva); EUDEM2_SOUTH_AMERICA (Fr_Guiana). EU-DEM v1.1 upgrade was coordinated by the European Environment Agency (EEA) in the frame of the EU Copernicus programme.
Property | Value |
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Spatial extent | [-54.925613, -21.567515, 93.178583, 71.89922] |
Temporal extent | 2016/04/20 - Current |
Copernicus Global 30 meter Digital Elevation Model dataset in COG format
The Copernicus DEM is a Digital Surface Model (DSM) which represents the surface of the Earth including buildings, infrastructure and vegetation. GLO-30 provides worldwide coverage at 30 meters (refers to 10 arc seconds). Note that ocean areas do not have tiles, there one can assume height values equal to zero. Data is provided as Cloud Optimized GeoTIFFs. Note that the vertical unit for measurement of elevation height is meters. The Copernicus DEM GLO-30 is mirrored from Open Data on AWS, dataset managed by Sinergise. https://registry.opendata.aws/copernicus-dem/.
Naming convention
Copernicus_DSM_COG_[resolution][northing][easting]_DEM/ * [resolution] = resolution in arc seconds (not meters!), which is 10 for GLO-30, and 30 for GLO-90. * [northing] = e.g. S50_00 - decimal degrees where the decimal part is always 00. In original files, this is the northing of the center of the bottom-most pixels, while in our files, because we removed the bottom-most pixels, the center of the new bottom-most pixels is one pixel-length (resolution) away to the north. * [easting] = e.g. w125_00 - decimal degrees where the decimal part is always 00. The easting of of the center of the left-most pixels.
For example: //copernicus-dem-90m/Copernicus_DSM_COG_30_S90_00_W178_00_DEM/
Property | Value |
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Spatial extent | [-180.0, -90.0, 180.0, 90.0] |
Temporal extent | 2021/03/03 - Current |
Copernicus Global 90 meter Digital Elevation Model dataset in COG format
The Copernicus DEM is a Digital Surface Model (DSM) which represents the surface of the Earth including buildings, infrastructure and vegetation. GLO-90 provides worldwide coverage at 90 meters (refers to 30 arc seconds). Note that ocean areas do not have tiles, there one can assume height values equal to zero. Data is provided as Cloud Optimized GeoTIFFs. Note that the vertical unit for measurement of elevation height is meters. The Copernicus DEM GLO-90 is mirrored from Open Data on AWS, dataset managed by Sinergise. https://registry.opendata.aws/copernicus-dem/.
Naming convention
Copernicus_DSM_COG_[resolution][northing][easting]_DEM/ * [resolution] = resolution in arc seconds (not meters!), which is 10 for GLO-30, and 30 for GLO-90. * [northing] = e.g. S50_00 - decimal degrees where the decimal part is always 00. In original files, this is the northing of the center of the bottom-most pixels, while in our files, because we removed the bottom-most pixels, the center of the new bottom-most pixels is one pixel-length (resolution) away to the north. * [easting] = e.g. w125_00 - decimal degrees where the decimal part is always 00. The easting of of the center of the left-most pixels.
For example: //copernicus-dem-90m/Copernicus_DSM_COG_30_S90_00_W178_00_DEM/
Property | Value |
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Spatial extent | [-180.0, -90.0, 180.0, 90.0] |
Temporal extent | 2021/03/03 - Current |
MapEO Water Chlorophyll-a (CHL) Products - V1
Optical data collected with airborne drone platform, and processed with MapEO Water software v1 at VITO into chlorophyll-a concentrations. Chlorophyll-a is a green pigment found in plants. It absorbs sunlight and converts it into sugar during photosynthesis. Chlorophyll-a concentrations are an indicator of phytoplankton abundance and biomass in inland, coastal, and estuarine waters. CHL is expressed in μg L-1 or mg m-3.
Property | Value |
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Spatial extent | [-180.0, -84.0, 180.0, 84.0] |
Temporal extent | 2018/02/01 - Current |
MapEO Water Water-Leaving Reflectance (RHOW) Products - V1
Optical data collected with airborne drone platform, and processed with MapEO Water software v1 at VITO into water-leaving reflectance. This is a geometrically and atmospherically corrected reflectance product.
Property | Value |
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Spatial extent | [-180.0, -84.0, 180.0, 84.0] |
Temporal extent | 2018/02/01 - Current |
MapEO Water Suspended Particulate Matter (SPM) Products - V1
Optical data collected with airborne drone platform, and processed with MapEO Water software v1 at VITO into suspended particulate matter concentrations. Suspended Particulate Matter concentration is the mass concentration of nano-scale to sand-size particles suspended in the water column. Some particles are present naturally in water, such as plankton, fine plant debris, and minerals (sand, silt or clay), while others originate from human activity (organic and inorganic matter). SPM is expressed in mg L-1 or g m-3.
Property | Value |
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Spatial extent | [-180.0, -84.0, 180.0, 84.0] |
Temporal extent | 2018/02/01 - Current |
MapEO Water Turbidity (TUR) Products - V1
Optical data collected with airborne drone platform, and processed with MapEO Water software v1 at VITO into turbidity. Turbidity indicates the relative opacity of the water column. It is an optical water property and a measure for the amount of light scattered by constituents in the water column. The higher the scattered light intensity, the higher the turbidity. Constituents that causes water to be turbid include clay, silt, very tiny inorganic and organic matter, algae, dissolved coloured organic compounds, plankton, and other microscopic organisms. Turbidity is expressed in Formazin Nephelometric Units (FNU, according to the ISO 7027 standard).
Property | Value |
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Spatial extent | [-180.0, -84.0, 180.0, 84.0] |
Temporal extent | 2018/02/01 - Current |