CLIMATIC FIELDS OF HORIZONTAL TEMPERATURE GRADIENTS OF WATER IN THE SOUTH ATLANTIC

dc.contributor.author	Galerkin L.I.
dc.contributor.author	Gritsenko A.M.
dc.contributor.author	Panfilova S.G.
dc.date.accessioned	2024-10-19T07:54:45Z
dc.date.available	2024-10-19T07:54:45Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13505420
dc.identifier.citation	Doklady Earth Sciences, 2006, 408, 4, 607-611
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46056
dc.description.abstract	The vertical structure of ocean water has been sufficiently well studied at present. Its principal elements—layers of discontinuity, warm and cold layers, saline and fresh layers, and their statistic and extreme characteristics—are known at all spatial and temporal scales. The horizontal structure of hydrophysical fields in oceans is less understood. Investigations were mainly restricted to the compilation of maps of temperature, salinity, density, and calculated currents.
dc.title	CLIMATIC FIELDS OF HORIZONTAL TEMPERATURE GRADIENTS OF WATER IN THE SOUTH ATLANTIC
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06040222

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