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During winter 1974–75, band-like ice features were observed via satellite in the Bering Sea water-ice transition zone during periods of off-ice winds. These were several tens of kilometers long, spaced from 6–12 km apart, and were generally oriented from 40–90° left of the surface wind direction. Formation of these features appears to be related to atmospheric convective processes; such features may he significant indicators of transition zone ice dynamics.
During winter 1974–75, band-like ice features were observed via satellite in the Bering Sea water-ice transition zone during periods of off-ice winds. These were several tens of kilometers long, spaced from 6–12 km apart, and were generally oriented from 40–90° left of the surface wind direction. Formation of these features appears to be related to atmospheric convective processes; such features may he significant indicators of transition zone ice dynamics.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 362 | 151 | 11 |
| PDF Downloads | 53 | 22 | 2 |
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