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dc.contributor.authorSaafani, M.A.A.
dc.contributor.authorShenoi, S.S.C.
dc.date.accessioned2006-09-05T06:32:12Z
dc.date.available2006-09-05T06:32:12Z
dc.date.issued2004
dc.identifier.citationProc. Indian Acad. Sci. (Earth Planet. Sci.), vol.113(3) 269-280p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/369
dc.description.abstractThe seasonal cycle of temperature - salinity variations in the Bab el Mandab region (southern Red Sea) is described using CTD data collected during four cruises spread over the period May 1995 { August 1997. A two layer system exists during early summer, winter and spring while a three layer system exists during summer. During summer, a large amount of the Gulf of Aden water intrudes into the Bab el Mandab region; up to the northern limit (14:5ºN). The quantity of Red Sea water that flows into the Gulf of Aden is maximum during the winter and minimum during the summer.
dc.format.extent1632613 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen
dc.publisherIndian Academy of Sciences
dc.subjectBab el Mandab
dc.subjectGulf of Aden
dc.titleSeasonal cycle of hydrography in the Bab el Mandab region, southern Red Sea
dc.typeJournal Article


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