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...

Full description

Bibliographic Details
Main Authors: Vowinckel,E., Taylor,Bea
Other Authors: MCGILL UNIV MONTREAL (QUEBEC)
Format: Text
Language:English
Published: 1964
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0600015
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0600015