{"type": "FeatureCollection", "features": [{"id": "0d0093fa-15e4-4b6a-b7cc-3f3a56fad431", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[34.4, 29.18], [34.4, 33.6], [36.8, 33.6], [36.8, 29.18], [34.4, 29.18]]]}, "properties": {"themes": [{"concepts": [{"id": "geoscientificInformation"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Asia"}, {"id": "Jordan"}], "scheme": "Continents, countries, sea regions of the world."}], "updated": "2022-05-30T12:40:40", "language": "eng", "title": "Incremental evapotranspiration (Jordan River Basin - Monthly - 100m)", "description": "Incremental evapotranspiration calculated for the Jordan River Basin area. The incremental evapotranspiration is part of the actual evapotranspiration and Interception (ETIa) that is not satified from precipitation but from supply or runoff from other cells or from groundwater. 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The evapotranspiration from precipitation (etrain) is the evapotranspiration of green water, in other words the fraction of the total evapotranspiration that is due to rainfall, calculated on a pixel-based soil moisture balance model. 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The incremental evapotranspiration (ETINCR) is the evapotranspriation of blue water, in other words the incremental evapotranspiration is the fraction of the total actual evapotranspiration that is not due to rainfall. The calculation of Incremental Evapotranspiration is based on a pixel-based soil moisture balance model. 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