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  The purpose of the Wind Scatterometer is to obtain information on wind speed and direction at the sea surface for incorporation into models, global statistics and climatological datasets. It operates by recording the change in radar reflectivity of the sea due to the perturbation of small ripples by the wind close to the surface. This is possible because the radar backscatter returned to the satellite is modified by wind-driven ripples on the ocean surface and, since the energy in these ripples increases with wind velocity, backscatter increases with wind velocity.
   
StatusOperational
 
TypeScatterometers
 
Technical Characteristics
Accuracy Sea surface wind speed: 3m/s, Sea ice type: 2 classes
Spatial Resolution Cells of 50km x 50km at 25km intervals
Swath Width 500km
Waveband Microwave: 5.3GHz (C-band), VV polarisation
 
ApplicationsAtmosphere (Winds) Natural Disasters (Hurricane)
 
Related Instruments
 
Latest Mission Operations     News
O'Higgins (TF), Antarctica - acquisition campaign

An ERS-2 acquisition campaign is foreseen for the following period:

12 January - 15 February 2010

The baseline planning is available in the catalogue.
Additional requests should be submitted through EOLI-SA according to the normal procedure.
 
Latest Data Product SCATTEROMETER Nominal Resolution Ocean Wind field and Sea Ice probability
 
Available Resources
Type
Access
Database of Global C-Band Radarbackscatter SoftwareOrder
Cyclic Acquisitions HTML
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