Search results
Results from the WOW.Com Content Network
Use of NASA logos, insignia and emblems is restricted per U.S. law 14 CFR 1221.; The NASA website hosts a large number of images from the Soviet/Russian space agency, and other non-American space agencies.
Nile basin water balance Global distribution of water balance in the soil averaged over the years 1981-2010 from the CHELSA-BIOCLIM+ data set [1]. The law of water balance states that the inflows to any water system or area is equal to its outflows plus change in storage during a time interval.
The main water supplier for the basin is Lake Victoria, located in the Great Rift Valley. [4] About 238 million people live within the Nile basin, 172 million of those inhabit rural localities. [5] In the southwestern part of the basin in South Sudan near the watershed with Congo Basin relief is made up a single large pediplain. [6]
The global annual runoff into the oceans (38,500–44,200 km 3 /year) is dominated by runoff into the South Atlantic from eastern South America, into the western Pacific from east Asia, and into the Indian Ocean from India, and southeast Asia.
Treaties have resulted in inequitable rights to the use of Nile water between the countries of the Nile Basin. April 15, 1891 – Article III of the Anglo-Italian Protocol. Article III states that "the Italian government engages not to construct on the Atbara River, in view of irrigation, any work which might sensibly modify its flow into the ...
WaterGAP has been applied to assess which areas of the world are and will be affected by water stress, and to estimate the world's freshwater balance. [3] In many studies, WaterGAP served to estimate the impact of climate change on the global freshwater system, e.g. on groundwater, [ 27 ] [ 28 ] [ 29 ] wetlands, [ 30 ] streamflow [ 31 ] [ 32 ...
The Nile runs through Sudan, South Sudan, Burundi, Rwanda, Democratic Republic of the Congo, Tanzania, Kenya, Uganda, Ethiopia, and Egypt and is considered to be the longest river in the world. The Nile is the only significant source of water in North Africa and 40% of Africa’s population lives in the Nile River Basin. [3]
Water balance. Groundwater recharge or deep drainage or deep percolation is a hydrologic process, where water moves downward from surface water to groundwater. Recharge is the primary method through which water enters an aquifer. This process usually occurs in the vadose zone below plant roots and is often expressed as a flux to the water table ...