EVAPORATION AND SENSIBLE HEAT FLUX OVER THE ARCTIC OCEAN.
These fluxes were calculated for each month over the Polar Ocean and the Norwegian-Barents Sea. Sverdrup's evaporation formula was used, and it was first examined how the K-coefficient in that formula depends on the wind speed frequency distribution. Seasonal maps were constructed of mean wind...
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Format: | Text |
Language: | English |
Published: |
1964
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Online Access: | http://www.dtic.mil/docs/citations/AD0600015 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0600015 |