Relating the Radar Return and Wind Speed

This panel shows an example of how wind speed and the radar return ("sigma0" on the left axis) are related for a variety of angles between the satellite and the sea surface.  Low returns (low sigma0) occur at low wind speeds.  High returns (high sigma0) occur at high wind speeds.  This wind speed model function is calibrated by comparing with independent measurements of ocean winds from ships or ocean buoys.