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Climatological shears between ship winds and satellite-observed, low-level cloud motions are used to derive monthly mean surface winds from satellite observations of low-level cloud drift. The derived surface winds compare well with observed surface winds from ships, moored buoys and the Seasat altimeter.
Climatological shears between ship winds and satellite-observed, low-level cloud motions are used to derive monthly mean surface winds from satellite observations of low-level cloud drift. The derived surface winds compare well with observed surface winds from ships, moored buoys and the Seasat altimeter.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 150 | 34 | 4 |
| PDF Downloads | 128 | 115 | 3 |
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