The Influence of the NORDKAPP (North Cape) Current on the Iciness of the Barents Sea (O Vliyanii Nordkapskogo Techeniya na Ledovitost Varentseva Morya)

The article substantiates empirical relations between the temperature of the active water layer in the axis of the Nordkapp Current and the general iciness of the Barents Sea in the following spring months. (Author) Trans. of Gosudarstvennyi Okeanograficheskii Institut. Trudy (USSR) n37 p14-33 1959,...

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Bibliographic Details
Main Author: Uralov,N. S.
Other Authors: NAVAL OCEANOGRAPHIC OFFICE WASHINGTON D C
Format: Text
Language:English
Published: 1961
Subjects:
Physical and Dynamic Oceanography
Snow
Ice and Permafrost
(*OCEAN CURRENTS
SEA ICE)
(*SEA ICE
*ARCTIC OCEAN)
SURFACE TEMPERATURE
SALINITY
HEAT FLUX
COOLING
HEAT TRANSFER
ATMOSPHERIC TEMPERATURE
CORRELATION TECHNIQUES
MARINE METEOROLOGY
USSR
*AIR WATER INTERACTIONS
*BARENTS SEA
TRANSLATIONS
Arctic
Arctic Ocean
Barents Sea
North Cape
Ice
Nordkapp
permafrost
Sea ice
Online Access:http://www.dtic.mil/docs/citations/AD0720153
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0720153
Description
Summary:The article substantiates empirical relations between the temperature of the active water layer in the axis of the Nordkapp Current and the general iciness of the Barents Sea in the following spring months. (Author) Trans. of Gosudarstvennyi Okeanograficheskii Institut. Trudy (USSR) n37 p14-33 1959, by M. Slessers. Also available as TT-61-28001.

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