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Precipitation minus evapotranspiration (Tigris and Euphrates River Basins - Monthly -250m)
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:... -
Incremental evapotranspiration (Tigris and Euphrates River Basins - Monthly -250m)
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.... -
Evapotranspiration from precipitation (Tigris and Euphrates River Basins - Monthly -250m)
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... -
Incremental evapotranspiration (Selenga, Mongolia - Monthly - 500m)
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... -
Evapotranspiration from precipitation (Selenga, Mongolia - Monthly - 500m)
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 (Litani River Basin, Lebanon - Monthly - 100m)
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 (Nile River Basin - Monthly - 100m)
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... -
Incremental evapotranspiration (Nile River Basin - Monthly - 100m)
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... -
Evapotranspiration from precipitation (Nile River Basin - Monthly - 100m)
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,... -
Number of rainy days in a month (Nile River Basin - Monthly - 100m)
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... -
Surface runoff (Litani River Basin, Lebanon - Monthly - 100m)
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 (Awash, Ethiopia - Monthly - 100m)
Precipitation minus actual evapotranspiration (P-ET) calculated over the Awash River basin area in Ethiopia. The P-ET is the difference between WaPOR precipitation (based on CHIRPS) and the actual... -
Precipitation minus actual evapotranspiration (Jordan River Basin - Monthly - 100m)
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... -
Evapotranspiration from precipitation (Awash, Ethiopia - Monthly -100m)
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 (Jordan River Basin - Monthly - 100m)
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... -
Evapotranspiration from precipitation (Jordan River Basin - Monthly - 100m)
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 (Litani River Basin, Lebanon - Monthly -100m)
Incremental evapotranspiration calculated for the Litani River Basin area. The incremental evapotranspiration (ETINCR) is the evapotranspriation of blue water, in other words the incremental... -
Incremental evapotranspiration (Awash, Ethiopia - Monthly - 100m)
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... -
Evapotranspiration from precipitation (Litani River Basin, Lebanon - Monthly - 100m)
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 (Litani River Basin, Lebanon - Monthly - 100m)
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...
