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A treasure trove of information

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Satellite altimetry is used to acquire sea-surface height measurements that yield information about:

Ocean properties:
Dynamic topography. Credits: CNES

Dynamic topography. Credits: CNES

The satellite gathers data on any point of the ocean surface. But measurements also contain a treasure trove of information about the entire water column, from the surface to the sea floor, including current speed and direction, wave heights and wind speed.



Oceanographers use these data to chart currents, study ocean seasons, improve knowledge of tides, monitor mean sea level and detect climate anomalies such as .
 

The MERCATOR system, in service since 2001, produces weekly 3-D analyses and ocean state forecasts out to 2 weeks, providing maps of currents, dynamic topography, salinity and temperature.

The MERCATOR system, in service since 2001, produces weekly 3-D analyses and ocean state forecasts out to 2 weeks, providing maps of currents, dynamic topography, salinity and temperature.

The ocean floor:
The geoid. Crédits : CNES

The geoid. Crédits : CNES

The topography of the ocean surface mirrors the bottom topography, albeit in attenuated form. A bump in the surface may correspond to a volcano or sea-mount, which creates a pocket of higher gravity that in turn leads to a build-up of a deeper layer of water.
Altimetry therefore allows us, indirectly, to obtain a picture of the geoid and is also useful in geophysics and geodesy for studying the physical properties of the solid Earth.


 
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