Structure and heat content of the West Spitsbergen Current

The seasonal evolution of the hydrographic structure of the West Spitsbergen Current (WSC) above bottom depths from 300 m to 800 m is discussed based on a modern data set with high spatial resolution. The WSC appears to have a core with high temperature and salinity, linked to the topography in this...

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Bibliographic Details
Published inPolar Research Vol. 18; no. 2; pp. 183 - 188
Main Author Haugan, Peter M.
Format Journal Article Conference Proceeding
LanguageEnglish
Published Oxford, UK Blackwell Publishing Ltd 01.12.1999
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