Boundary of the Tigris and Euphrates River Basins obtained from HydroBASINS (Lerner and Grill, 2013). Data publication: 2023-01-25 Contact points: Resource Contact: Solomon Seyoum Metadata Contact:...

Precipitation minus actual evapotranspiration (P-ET) calculated over the Litani River Basin area in Lebanon. The P-ET is the difference between WaPOR precipitation (based on CHIRPS) and the actual...

Saturated soil water content calculated over the Jordan River Basin area in Jordan. The dataset is derived from the High Resolution Soil Map of Hydraulic Properties (HiHydroSoils v1.0). Data...

Saturated soil water content calculated over the Litani River Basin area in Lebanon. The dataset is derived from the High Resolution Soil Map of Hydraulic Properties (HiHydroSoils v1.0). Data...

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....

Precipitation minus actual evapotranspiration (P-ET) calculated over the Jordan River Basin area. The P-ET is the difference between WaPOR precipitation (based on CHIRPS) and the actual...

The evapotranspiration from precipitation (ETRAIN) is the portion of the actual evapotranspiration and Interception (ETIa) that is satified from precipitation. It is computed from precipitation,...

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...

The evapotranspiration from precipitation (ETRAIN) is the portion of the actual evapotranspiration and Interception (ETIa) that is satified from precipitation. It is computed from precipitation,...

Incremental evapotranspiration calculated for the Litani River Basin area. The incremental evapotranspiration (ETINCR) is the evapotranspriation of blue water, in other words the incremental...

Evapotranspiration from precipitation calculated over the Litani River Basin area. The evapotranspiration from precipitation (etrain) is the evapotranspiration of green water, in other words the...

Base flow calculated for the Litani River Basin area in Lebanon. Base flow (bf) or slow flow is the component of the total flow that is due to groundwater discharge. It mainly occurs during dry...

Total flow calculated over the Litani River Basin area in Lebanon. The total flow (tf) is the sum of surface runoff (sro) and the base flow (bf). More information can be found on the Water...

Percolation calculated Litani River Basin area in Lebanon. The percolation (perco) is the amount of soil moisture in the root zone that leaks deeper contributing to groundwater recharge. The...

Supplied water calculated over the Litani River Basin area. The supplied water is the amount of water that is artificially or naturally supplied to a pixel generating incremental evapotranspiration...

Number of rainy days calculated in the Litani River Basin area. For every pixel, the number of rainy days in a month is reported. This dataset is created by using daily rainfall data from the...

This land use dataset, covering the Litani River Basin area, is based on the land cover classification map of 2013 produced by the National Center for Remote Sensing, (CNRS), Lebanon. The...

Boundary of the Litani River Basin obtained from HydroBASINS (Lerner and Grill, 2013). Data publication: 2019-07 Contact points: Metadata Contact: Bich Tran Data lineage: Contact WWF Hydrosheds for...

Boundary of the Jordan River Basin obtained from HydroBASINS (Lerner and Grill, 2013). Data publication: 2019-07-01 Contact points: Metadata Contact: Solomon Seyoum Data lineage: Contact WWF...

Awash river basin boundary is derived from the HydroBASINS product, which was obtained by delineating drainage basin boundaries from hydrologically corrected elevation data (WWF HydroSHEDS, Lehner...