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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Bibliographic Details
Main Author: Bilello,Michael A.
Other Authors: SNOW ICE AND PERMAFROST RESEARCH ESTABLISHMENT WILMETTE ILL
Format: Text
Language:English
Published: 1961
Subjects:
Rho
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0653136
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0653136