{"type": "FeatureCollection", "features": [{"id": "23364050-f918-4cf3-9adf-6f7348c21c5e", "type": "Feature", "geometry": {"type": "Polygon", "coordinates": [[[35.2, 33.09], [35.2, 34.06], [36.4, 34.06], [36.4, 33.09], [35.2, 33.09]]]}, "properties": {"themes": [{"concepts": [{"id": "geoscientificInformation"}], "scheme": "https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_TopicCategoryCode"}, {"concepts": [{"id": "Asia"}], "scheme": "Continents, countries, sea regions of the world."}], "updated": "2022-05-31T07:50:37", "language": "eng", "title": "Surface Runoff (Litani River Basin, Lebanon - Monthly - 100m)", "description": "Surface runoff calculated for the Litani River Basin area. The surface runoff (sro) is the fraction of the effective rainfall that does infiltrate into the soil and contributes to overland flow. 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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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Base flow (bf) or slow flow is the component of the total flow that is due to groundwater discharge. It mainly occurs during dry months. The calculation of base flow is based on a pixel-based soil water 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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The percolation (perco) is the amount of soil moisture in the root zone that leaks deeper contributing to groundwater recharge. The calculation of percolation is based on a pixel-based soil moisture balance model. 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