Principle: |
The calibration coefficient
is estimated over sea based on the knowledge we have of the Normalized
Radar Cross Section (level and behavior) with respect of geophysical
(ocean Surface wind speed and direction relative to antenna look angle)
and radar (polarization, incidence angle) parameters. |
NRCS vs Wind model | NRCS vs incidence |
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SM2 |
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SM3 |
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SM4 |
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SM5 |
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SM6 |
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EW map |
EW NRCS vs Wind |
EW NRCS vs incidence |
IW map |
IW NRCS vs Wind |
IW NRCS vs incidence |
Contact: |
A. Grouazel |