Reduction of weather effects in the calculation of sea-ice concentration with the DMSP SSM/I
A problem in mapping the polar sea-ice covers in both hemispheres has been the sporadic false indication of sea ice over the open ocean and at the ice edge. These spurious sea-ice concentrations result from variations in sea-surface roughening by surface winds, atmospheric water vapor and both preci...
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Veröffentlicht in: | Journal of glaciology 1995, Vol.41 (139), p.455-464 |
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Sprache: | eng |
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