SPREADING OF DENSE SHELF WATER IN THE DEEP SEA OF OKHOTSK

dc.contributor.author	Gladyshev S.V.
dc.contributor.author	Khen G.V.
dc.date.accessioned	2022-07-18T05:29:16Z
dc.date.available	2022-07-18T05:29:16Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13453066
dc.identifier.citation	Doklady Earth Sciences, 2004, 398, 7, 953-956
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38255
dc.description.abstract	The 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.title	SPREADING OF DENSE SHELF WATER IN THE DEEP SEA OF OKHOTSK
dc.type	Статья

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