Sea ice melting in the marginal ice zone.

Journal of Geophysical Research


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The heat and salt flux boundary conditions together with the freezing curve relationship are a necessary component of any ice- sea water thermodynamic model. A neutral two-layer oceanic planetary boundary layer model that incorporates these boundary conditions is used. The results are discussed. -from Author
Publication type Article
Publication Subtype Journal Article
Title Sea ice melting in the marginal ice zone.
Series title Journal of Geophysical Research
Volume 88
Issue C5
Year Published 1983
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Journal of Geophysical Research
First page 2841
Last page 2844
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