STRUCTURE AND VARIABILITY OF DEEP WATERS IN THE ROMANCHE FRACTURE ZONE

dc.contributor.author	Demidov A.N.
dc.contributor.author	Morozov E.G.
dc.contributor.author	Neiman V.G.
dc.date.accessioned	2024-10-23T07:15:47Z
dc.date.available	2024-10-23T07:15:47Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13507248
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1136-1140
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46116
dc.description.abstract	Hydrophysical measurements in the Romanche Fracture Zone carried out in October 2005 were compared to the data of measurements in 1991. As a result, warming by 0.01°C was found in the core of North Atlantic Deep Water (NADW), and warming by 0.034 °C was recorded in the layer of Antarctic Bottom Water (AABW). Our results confirmed the conclusions of Mantyla and Reid, according to which the major part of AABW passes to the Northeast Atlantic not through the Romanche Fracture Zone but through the Vema Fracture Zone at 11° N.
dc.title	STRUCTURE AND VARIABILITY OF DEEP WATERS IN THE ROMANCHE FRACTURE ZONE
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070300

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