Sea ice melting in the marginal ice zone.
Journal of Geophysical Research
By: E.G. Josberger
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Abstract
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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