Boundary-Layer Structure Near an Ice Edge as a Function of Wind Direction
This paper examines the Sensitivity of boundary-layer (BL) frontal' features, created by differences across an ice edge and characterized by positive vertical velocity (w), to variations in geostrophic wind direction (a), particularly for flow approximately parallel to the ice edge. Notable is...
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Format: | Text |
Language: | English |
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1992
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Online Access: | http://www.dtic.mil/docs/citations/ADA268437 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA268437 |