Sea ice melting in the marginal ice zone.
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
Citation Information
Publication Year | 1983 |
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Title | Sea ice melting in the marginal ice zone. |
Authors | E.G. Josberger |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Journal of Geophysical Research |
Index ID | 70012038 |
Record Source | USGS Publications Warehouse |