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Earth's water cycle. Powered by the Sun, the Earth's finite water supply is continuously being circulated between the oceans, the atmosphere and the land. This circulation and conservation of Earth's water is a crucial component of our weather and climate.

Credits: ESA - AOES Medialab
 
 
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Animation of the energy and water balance of the physical climate system including terrestrial and atmospheric components of the water cycle.

Credits: ESA - AOES Medialab
 
 
Map showing average distribution of sea-surface salinity values. Areas of red indicate regions of high salinity, and areas of green indicate regions of low salinity. The map is overlaid with the simplified global circulation pattern called the 'thermohaline circulation'. The blue arrows indicate cool deeper currents and the red indicate wamer surface currents. Temperature (thermal) and salinity (haline) variations are key variables affecting ocean circulation.

Credits: ESA
 
 
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Temperature (thermo) and salinity (haline) variations are key variables affecting global ocean circulation patterns. The blue arrows indicated cool deeper currents and the red indicate warmer surface currents.

Credits: ESA/AOES Medialab
 
  Last update: 2 November 2010 
 
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More information
SMOS - ESA's water mission (BR-288)SMOS - la misión del agua de la ESA
(BR-278)
SMOS – mission de l'ESA dédiée au cycle de l'eau (BR-278)SMOS factsheet
Special features
SMOS: ESA's water mission
From a technological perspective
Technology leaps let SMOS follow Earth’s water
Related links
Thales Alenia SpaceCNESEADS-CASACESBIO SMOS pageIfremer-Cersat Salinity CenterGerman SMOS Project OfficeSMOS Barcelona Expert CentreSMOS Level 3/4 Processing Centre, SpainInternational Soil Moisture Network
 
 
 
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