SPREADING OF DENSE SHELF WATER IN THE DEEP SEA OF OKHOTSK

dc.contributor.authorGladyshev S.V.
dc.contributor.authorKhen G.V.
dc.date.accessioned2022-07-18T05:29:16Z
dc.date.available2022-07-18T05:29:16Z
dc.date.issued2004
dc.description.abstractThe MDSW represents a powerful and the most significant factor responsible for ventilation (consequently, formation and variability) of the intermediate water mass of the North Pacific. The main purpose of this work is a calculation of new thermohaline indices of the MDSW and discussion of its spreading patterns and mixing in the Sea of Okhotsk.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13453066
dc.identifier.citationDoklady Earth Sciences, 2004, 398, 7, 953-956
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/38255
dc.titleSPREADING OF DENSE SHELF WATER IN THE DEEP SEA OF OKHOTSK
dc.typeСтатья

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