JRC-IES-GMIS
eng
dataset
Institute for Environment and Sustainability, Joint Research Centre
JRC-EMIS@ec.europa.eu
pointOfContact
2013-12-12
ISO19115
2003/Cor.1:2006
GMIS - List of Web services
2013-12-12
creation
Global Marine Information System
Global Marine Information System, Directorate D - Sustainable Resources, Joint Research Centre
JRC-EMIS@ec.europa.eu
pointOfContact
infoMapAccessService
ISO - 19119 geographic services taxonomy
2010-01-19
publication
ocean color
satellite observations
marine environment
coastal environment
sea water protection
marine monitoring
GIS digital format
climate change
Environmental monitoring facilities
Oceanographic geographical features
Protected sites
GEMET - INSPIRE themes, version 1.0
2008-06-01
publication
environmental data
GEMET - Concepts, version 2.4
2010-01-13
publication
HYDROSPHERE (freshwater, marine water, waters)
GEMET - Groups, version 2.4
2010-01-13
publication
NATURAL ENVIRONMENT, ANTHROPIC ENVIRONMENT
GEMET - Supergroups, version 2.4
2010-01-13
publication
water
GEMET - Themes, version 2.4
2010-01-13
publication
OCEANS
GEOSS - Earth Observation Vocabulary, version 1.0
2011-05-01
publication
no conditions apply
otherRestrictions
no limitation
1981-09-01
unknown
unknown
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/modisa/?DATASET=chla
GMIS - MODIS-AQUA Monthly mean sea surface Chlorophyll-a concentration (9km)
Algal biomass (chlorophyll concentration, Chla in mg.m-3): Chlorophyll is a photosynthetic pigment commonly present in all phytoplankton species. It is used as a proxy for phytoplankton biomass. Chlorophyll concentration is a standard product from satellite-based optical sensors, usually retrieved from empirical algorithms using reflectance ratios at two or more wavebands.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/modisa/?DATASET=kd490
GMIS - MODIS-AQUA Monthly mean sea surface diffuse attenuation coefficient (9km)
Water Transparency (Diffuse attenuation coefficient at 490nm, Kd490 in m-1): The diffuse attenuation coefficient Kd490 measures the light penetration in the water column at the blue-green wavelengths (ca. 490 nm). It represents a good indicator of water transparency resulting from the combined action of absorption and backscattering by the water constituents, and the structure of the surrounding light field.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/modisa/?DATASET=par
GMIS - MODIS-AQUA Monthly mean photosynthetically available radiation (9km)
Photosynthetically Active Radiation (PAR in Einstein.m-2.day-1): PAR is defined as the quantum energy flux from the sun in the spectral range 400 to 700 nm, usable in the process of photosynthesis by phytoplankton, benthic algae and seagrass.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/modisa/?DATASET=aph
GMIS - MODIS-AQUA Monthly mean absorption coefficient due to phytoplankton (9km)
Absorption Coefficient of Phytoplankton at 443nm (aph in m-1): The absorption coefficient aph represents the fraction of incident light absorbed by phytoplankton organisms. It is an index of variability of the phytoplankton biomass in marine and coastal turbid waters.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/modisa/?DATASET=adg
GMIS - MODIS-AQUA Monthly mean absorption coefficient due to chromophoric dissolved organic matter and non-pigmented particles (4km)
Absorption Coefficient of colored detrital matter at 443nm (adg in m-1): The absorption coefficient adg represents the fraction of incident light absorbed by both detrital particles and colored dissolved organic matter (CDOM). Dissolved organic matter is an important component of the oceanic carbon cycle. It is also used as proxy to assess the impact of terrigenous inputs in coastal waters.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/modisa/?DATASET=bbp
GMIS - MODIS-AQUA Monthly mean particulate backscattering coefficient (9km)
Particulate matter (particulate backscatter coefficient at 443 nm, bbp in m-1): The backscatter coefficient bbp represents the fraction of incident light that is scattered backward from its original path. The backscattering coefficient gives a good indication of the concentration of suspended organic and inorganic particles (e.g. sediments) in the water.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/seawifs/?DATASET=chla
GMIS - SeaWiFS Monthly mean sea surface Chlorophyll-a concentration (9km)
Algal biomass (chlorophyll concentration, Chla in mg.m-3): Chlorophyll is a photosynthetic pigment commonly present in all phytoplankton species. It is used as a proxy for phytoplankton biomass. Chlorophyll concentration is a standard product from satellite-based optical sensors, usually retrieved from empirical algorithms using reflectance ratios at two or more wavebands.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/seawifs/?DATASET=kd490
GMIS - SeaWiFS Monthly mean sea surface diffuse attenuation coefficient (9km)
Water Transparency (Diffuse attenuation coefficient at 490nm, Kd490 in m-1): The diffuse attenuation coefficient Kd490 measures the light penetration in the water column at the blue-green wavelengths (ca. 490 nm). It represents a good indicator of water transparency resulting from the combined action of absorption and backscattering by the water constituents, and the structure of the surrounding light field.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/seawifs/?DATASET=pp
GMIS - SeaWiFS Monthly mean primary production (9km)
Water productivity (primary production, pp in gCarbon.m-2.day-1): The primary production represents the amount of organic carbon produced through phytoplankton photosynthesis. It is a critical element of the Earth's carbon budget and the marine food web. The depth-integrated primary production is modeled from the satellite-based phytoplankton biomass concentration and PAR.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/seawifs/?DATASET=par
GMIS - SeaWiFS Monthly mean photosynthetically available radiation (9km)
Photosynthetically Active Radiation (PAR in Einstein.m-2.day-1): PAR is defined as the quantum energy flux from the sun in the spectral range 400 to 700 nm, usable in the process of photosynthesis by phytoplankton, benthic algae and seagrass.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/seawifs/?DATASET=aph
GMIS - SeaWiFS Monthly mean absorption coefficient due to phytoplankton (9km)
Absorption Coefficient of Phytoplankton at 443nm (aph in m-1): The absorption coefficient aph represents the fraction of incident light absorbed by phytoplankton organisms. It is an index of variability of the phytoplankton biomass in marine and coastal turbid waters.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/seawifs/?DATASET=adg
GMIS - SeaWiFS Monthly mean absorption coefficient due to chromophoric dissolved organic matter and non-pigmented particles (9km)
Absorption Coefficient of colored detrital matter at 443nm (adg in m-1): The absorption coefficient adg represents the fraction of incident light absorbed by both detrital particles and colored dissolved organic matter (CDOM). Dissolved organic matter is an important component of the oceanic carbon cycle. It is also used as proxy to assess the impact of terrigenous inputs in coastal waters.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/seawifs/?DATASET=bbp
GMIS - SeaWiFS Monthly mean particulate backscattering coefficient (9km)
Particulate matter (particulate backscatter coefficient at 443 nm, bbp in m-1): The backscatter coefficient bbp represents the fraction of incident light that is scattered backward from its original path. The backscattering coefficient gives a good indication of the concentration of suspended organic and inorganic particles (e.g. sediments) in the water.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/meris/?DATASET=chla
GMIS - MERIS Monthly mean sea surface Chlorophyll-a concentration (9km)
Algal biomass (chlorophyll concentration, Chla in mg.m-3): Chlorophyll is a photosynthetic pigment commonly present in all phytoplankton species. It is used as a proxy for phytoplankton biomass. Chlorophyll concentration is a standard product from satellite-based optical sensors, usually retrieved from empirical algorithms using reflectance ratios at two or more wavebands.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/meris/?DATASET=kd490
GMIS - MERIS Monthly mean sea surface diffuse attenuation coefficient (9km)
Water Transparency (Diffuse attenuation coefficient at 490nm, Kd490 in m-1): The diffuse attenuation coefficient Kd490 measures the light penetration in the water column at the blue-green wavelengths (ca. 490 nm). It represents a good indicator of water transparency resulting from the combined action of absorption and backscattering by the water constituents, and the structure of the surrounding light field.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/modist/?DATASET=sst
GMIS - MODIS-TERRA Monthly mean sea surface temperature (9km)
Sea surface temperature (SST in degree-C): Sea surface temperature is the temperature of the water close to the sea surface. SST is a standard product from satellite-based thermal infra-red sensors, and optical sensors complemented with infrared bands.
view
http://gmis.jrc.ec.europa.eu/webservices/9km/wms/pathfinder/?DATASET=sst
GMIS - PATHFINDER Monthly mean sea surface temperature (9km)
Sea surface temperature (SST in degree-C): Sea surface temperature is the temperature of the water close to the sea surface. SST is a standard product from satellite-based thermal infra-red sensors, and optical sensors complemented with infrared bands.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/modisa/?DATASET=chla
GMIS - MODIS-AQUA Monthly mean sea surface Chlorophyll-a concentration (4km)
Algal biomass (chlorophyll concentration, Chla in mg.m-3): Chlorophyll is a photosynthetic pigment commonly present in all phytoplankton species. It is used as a proxy for phytoplankton biomass. Chlorophyll concentration is a standard product from satellite-based optical sensors, usually retrieved from empirical algorithms using reflectance ratios at two or more wavebands.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/modisa/?DATASET=kd490
GMIS - MODIS-AQUA Monthly mean sea surface diffuse attenuation coefficient (4km)
Water Transparency (Diffuse attenuation coefficient at 490nm, Kd490 in m-1): The diffuse attenuation coefficient Kd490 measures the light penetration in the water column at the blue-green wavelengths (ca. 490 nm). It represents a good indicator of water transparency resulting from the combined action of absorption and backscattering by the water constituents, and the structure of the surrounding light field.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/modisa/?DATASET=par
GMIS - MODIS-AQUA Monthly mean photosynthetically available radiation (4km)
Photosynthetically Active Radiation (PAR in Einstein.m-2.day-1): PAR is defined as the quantum energy flux from the sun in the spectral range 400 to 700 nm, usable in the process of photosynthesis by phytoplankton, benthic algae and seagrass.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/modisa/?DATASET=aph
GMIS - MODIS-AQUA Monthly mean absorption coefficient due to phytoplankton (4km)
Absorption Coefficient of Phytoplankton at 443nm (aph in m-1): The absorption coefficient aph represents the fraction of incident light absorbed by phytoplankton organisms. It is an index of variability of the phytoplankton biomass in marine and coastal turbid waters.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/modisa/?DATASET=adg
GMIS - MODIS-AQUA Monthly mean absorption coefficient due to chromophoric dissolved organic matter and non-pigmented particles (4km)
Absorption Coefficient of colored detrital matter at 443nm (adg in m-1): The absorption coefficient adg represents the fraction of incident light absorbed by both detrital particles and colored dissolved organic matter (CDOM). Dissolved organic matter is an important component of the oceanic carbon cycle. It is also used as proxy to assess the impact of terrigenous inputs in coastal waters.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/modisa/?DATASET=bbp
GMIS - MODIS-AQUA Monthly mean particulate backscattering coefficient (4km)
Particulate matter (particulate backscatter coefficient at 443 nm, bbp in m-1): The backscatter coefficient bbp represents the fraction of incident light that is scattered backward from its original path. The backscattering coefficient gives a good indication of the concentration of suspended organic and inorganic particles (e.g. sediments) in the water.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/seawifs/?DATASET=chla
GMIS - SeaWiFS Monthly mean sea surface Chlorophyll-a concentration (4km)
Algal biomass (chlorophyll concentration, Chla in mg.m-3): Chlorophyll is a photosynthetic pigment commonly present in all phytoplankton species. It is used as a proxy for phytoplankton biomass. Chlorophyll concentration is a standard product from satellite-based optical sensors, usually retrieved from empirical algorithms using reflectance ratios at two or more wavebands.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/seawifs/?DATASET=kd490
GMIS - SeaWiFS Monthly mean sea surface diffuse attenuation coefficient (4km)
Water Transparency (Diffuse attenuation coefficient at 490nm, Kd490 in m-1): The diffuse attenuation coefficient Kd490 measures the light penetration in the water column at the blue-green wavelengths (ca. 490 nm). It represents a good indicator of water transparency resulting from the combined action of absorption and backscattering by the water constituents, and the structure of the surrounding light field.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/seawifs/?DATASET=par
GMIS - SeaWiFS Monthly mean photosynthetically available radiation (4km)
Photosynthetically Active Radiation (PAR in Einstein.m-2.day-1): PAR is defined as the quantum energy flux from the sun in the spectral range 400 to 700 nm, usable in the process of photosynthesis by phytoplankton, benthic algae and seagrass.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/seawifs/?DATASET=aph
GMIS - SeaWiFS Monthly mean absorption coefficient due to phytoplankton (4km)
Absorption Coefficient of Phytoplankton at 443nm (aph in m-1): The absorption coefficient aph represents the fraction of incident light absorbed by phytoplankton organisms. It is an index of variability of the phytoplankton biomass in marine and coastal turbid waters.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/seawifs/?DATASET=adg
GMIS - SeaWiFS Monthly mean absorption coefficient due to chromophoric dissolved organic matter and non-pigmented particles (4km)
Absorption Coefficient of colored detrital matter at 443nm (adg in m-1): The absorption coefficient adg represents the fraction of incident light absorbed by both detrital particles and colored dissolved organic matter (CDOM). Dissolved organic matter is an important component of the oceanic carbon cycle. It is also used as proxy to assess the impact of terrigenous inputs in coastal waters.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/seawifs/?DATASET=bbp
GMIS - SeaWiFS Monthly mean particulate backscattering coefficient (4km)
Particulate matter (particulate backscatter coefficient at 443 nm, bbp in m-1): The backscatter coefficient bbp represents the fraction of incident light that is scattered backward from its original path. The backscattering coefficient gives a good indication of the concentration of suspended organic and inorganic particles (e.g. sediments) in the water.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/meris/?DATASET=chla
GMIS - MERIS Monthly mean sea surface Chlorophyll-a concentration (4km)
Algal biomass (chlorophyll concentration, Chla in mg.m-3): Chlorophyll is a photosynthetic pigment commonly present in all phytoplankton species. It is used as a proxy for phytoplankton biomass. Chlorophyll concentration is a standard product from satellite-based optical sensors, usually retrieved from empirical algorithms using reflectance ratios at two or more wavebands.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/meris/?DATASET=kd490
GMIS - MERIS Monthly mean sea surface diffuse attenuation coefficient (4km)
Water Transparency (Diffuse attenuation coefficient at 490nm, Kd490 in m-1): The diffuse attenuation coefficient Kd490 measures the light penetration in the water column at the blue-green wavelengths (ca. 490 nm). It represents a good indicator of water transparency resulting from the combined action of absorption and backscattering by the water constituents, and the structure of the surrounding light field.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/modist/?DATASET=sst
GMIS - MODIS-TERRA Monthly mean sea surface temperature (4km)
Sea surface temperature (SST in degree-C): Sea surface temperature is the temperature of the water close to the sea surface. SST is a standard product from satellite-based thermal infra-red sensors, and optical sensors complemented with infrared bands.
view
http://gmis.jrc.ec.europa.eu/webservices/4km/wms/pathfinder/?DATASET=sst
GMIS - PATHFINDER Monthly mean sea surface temperature (4km)
Sea surface temperature (SST in degree-C): Sea surface temperature is the temperature of the water close to the sea surface. SST is a standard product from satellite-based thermal infra-red sensors, and optical sensors complemented with infrared bands.
view
dataset
COMMISSION REGULATION (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services
2010-12-08
publication
See the referenced specification
false