ON THE STEADY-STATE FLOW OF SEA ICE.
The purpose of this paper is to create a model in which the ice and ocean are viewed as a dynamic unit and in which the gradient currents and internal ice stresses are included. Also, this paper is concerned with the solution of such a model.
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| Format: | Text |
| Language: | English |
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1964
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| Online Access: | http://www.dtic.mil/docs/citations/AD0604368 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0604368 |
| Summary: | The purpose of this paper is to create a model in which the ice and ocean are viewed as a dynamic unit and in which the gradient currents and internal ice stresses are included. Also, this paper is concerned with the solution of such a model. |
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