Concept information
Pas de terme dans cette langue pour ce concept
Terme préférentiel
Water cycle (en)
Type
-
https://w3id.org/iadopt/ont/Entity
Définition
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The water cycle, also known as the hydrologic cycle or the hydrological cycle, is a biogeochemical cycle that describes the continuous movement of water on, above and below the surface of the Earth. The mass of water on Earth remains fairly constant over time but the partitioning of the water into the major reservoirs of ice, fresh water, saline water (salt water) and atmospheric water is variable depending on a wide range of climatic variables. The water moves from one reservoir to another, such as from river to ocean, or from the ocean to the atmosphere, by the physical processes of evaporation, transpiration, condensation, precipitation, infiltration, surface runoff, and subsurface flow. In doing so, the water goes through different forms: liquid, solid (ice) and vapor. The ocean plays a key role in the water cycle as it is the source of 86% of global evaporation. (en)
Concept générique
- Phenomenon (en)
Concepts spécifiques
- Evapotranspiration (en)
- Groundwater flow (en)
- Groundwater recharge (en)
- Ice flow (en)
- Precipitation (en)
- Snowmelt (en)
- Streamflow (en)
- Surface runoff (en)
Traductions
-
anglais
URI
https://w3id.org/ozcar-theia/c_418b5b00
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