The land use map based on Water Accounting Plus land use classification is produced based on WaPOR land cover class and protected areas from the World Database on Protected Areas and reservoirs...

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 and Interception (P-ET) is the difference between WaPOR P and ETIa. Data publication: 2023-01-25 Supplemental Information: No data value: -9999 Unit:...

The blue 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....

The rainfall evapotranspiration is part of the actual EvapoTranspiration and Interception (ETIa) that is satified from precipitation. It is calculated by spliting ETIa to rainfall and blue ET...

The land use (LU) map based on Water Accounting Plus land use classification is produced based on WaPOR land cover class and protected areas from the World Database on Protected Areas. Please read...

Land Cover Classification covering the Nura-Sarysu Water Economic basin with complete drainage area of the Nura and Sarysu rivers and Lake Tengiz with buffer. This land cover dataset is based on...

Incremental Evapotranspiration calculated for the Mongolian Selenga Basin and the Selenga drainage area to Naushki, beyond the boundaries of Mongolia. The incremental evapotranspiration (etincr) is...

Land Cover Classification covering the Mongolian Selenga Basin and the Selenga drainage area to Naushki, beyond the boundaries of Mongolia. This land cover dataset is based on the Copernicus GLobal...

Evapotranspiration from precipitation calculated for the Mongolian Selenga Basin and the Selenga drainage area to Naushki, beyond the boundaries of Mongolia. The Evapotranspiration from...

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...

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

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...

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,...

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

Number of rainy days calculated in the Nile 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 WaPOR...

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

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....