SOME HYDRODYNAMIC PROBLEMS FOR A NEPHELOID ZONE.
A layer of a few hundred meters' thickness with suspended matter near the bottom on the continental slope of the North Atlantic (a nepheloid zone) discovered by Ewing and Thorndike seems to produce bottom currents, because heavier water near the bottom due to suspended matter slides down the sl...
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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/AD0610047 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0610047 |