Research news on water cycle

The water cycle, or hydrologic cycle, is the continuous circulation of water within the Earth–atmosphere system, driven primarily by solar radiation and gravity. It encompasses phase changes and fluxes such as evaporation and transpiration from surface and biotic reservoirs, condensation in the atmosphere, cloud formation, and subsequent precipitation as rain, snow, or other hydrometeors. Infiltration, percolation, and groundwater flow redistribute water within subsurface reservoirs, while surface runoff and riverine transport return water to oceans and lakes. The water cycle regulates climate, controls energy and mass exchanges, and governs biogeochemical transport across terrestrial, aquatic, and atmospheric compartments.

SMOS mission could offer early indicator of El Niño

Sea-surface salinity, the concentration of dissolved salts in the upper layer of the ocean, is much more than a measure of how salty the sea is. It responds rapidly to changes in rainfall, evaporation, river discharge and, ...

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