SURFACE TEMPERATURES AND GROWTH OF SEA ICE.
Sea-ice surface temperatures observed at Eureka, N.W.T., Canada, during 1949-50 and 1950-51 were used to compute the numerical value of the expression k/L rho, where k = thermal conductivity, L = latent heat of fusion and rho = density. The numerical value for these combined physical properties of s...
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Format: | Text |
Language: | English |
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1961
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Online Access: | http://www.dtic.mil/docs/citations/AD0653136 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0653136 |