ESA title
Altimetry-derived mean dynamic topography
Applications

About radar altimetry

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ESA / Applications / Observing the Earth

Radar altimeters measure the surface topography profile along the satellite track. They provide precise measurements of a satellite’s height above the ocean by measuring the time interval between the transmission and reception of very short electromagnetic pulses.

A variety of parameters may be inferred using the information from these measurements, such as time-varying sea-surface height (ocean topography), the thickness of sea ice and altitude of large icebergs above sea level, the levels of rivers and lakes, as well as the topography of land and ice sheets, and – indirectly – even that of the sea floor.

The 2012 event in Venice takes place just after the 20-year anniversary of the launch of the first European Remote Sensing satellite, ERS-1, and of the joint CNES and NASA mission TOPEX/Poseidon. Both missions carried radar altimeters. TOPEX/Poseidon was followed by the Jason-1 and -2 missions, flown in 2001 and 2008, respectively.

ESA’s follow-up instruments aboard ERS-2, Envisat and CryoSat have ensured the continuity of radar altimetry measurements. ESA will launch its next radar altimeters with the Sentinel-3 mission within Europe’s Global Monitoring for Environment and Security (GMES) programme.

About ESA’s Earth observation programme:
www.esa.int/eo

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