Ocean Mixing and Circulation Response in the Marginal Ice Zone.
A sea ice model using the Rossby-similarity method was added to a two-dimensional, embedded ocean general circulation--mixed layer model. Advection, diffusion, and mixing of buoyancy and momentum were included in the model to determine their effects on the ocean response. In particular, the case of...
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| Format: | Text |
| Language: | English |
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1983
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| Online Access: | http://www.dtic.mil/docs/citations/ADA132174 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA132174 |