Processes
The Hydrologic Cycle
Also Known As The Water Cycle
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A biogeochemical cycle that involves the continuous change in form of water on, above and below the surface of the Earth across different reservoirs. Evaporation lifts water into the atmosphere, condensation gathers it into clouds, and precipitation, rain, snow, hail and sleet, returns it to the surface, powered throughout by solar energy.
Facts
TimescaleContinuous, days for atmospheric water to thousands of years for deep groundwater 1 Driving ForceSolar energy, which evaporates water from the ocean and land surface, and gravity, which returns precipitation to the surface and drives its flow back to the sea. 1 Resulting FeatureContinuously moves water among the ocean, atmosphere, land surface, groundwater and ice, connecting evaporation, condensation, precipitation and runoff. 1 SignificanceThe hydrologic cycle supplies the fresh water on which all terrestrial life and agriculture depend, and its intensification is a major expected consequence of climate change. 1 Cross-Tradition Connections
Associated With
Groundwater is the subsurface leg of the hydrologic cycle that hydrogeology studies in detail.
Lakes and inland waters limnology studies are reservoirs within the hydrologic cycle.
The water cycle is a sibling among Earth's major biogeochemical cycles.
In Discipline
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