Flows of Bottom Water in Fractures of the North Mid-Atlantic Ridge

被引：2

作者：

Morozov, E. G. ^{[1
]}

Tarakanov, R. Yu. ^{[1
]}

Demidova, T. A. ^{[1
]}

Makarenko, N. I. ^{[2
]}

机构：

[1] Russian Acad Sci, Shirshov Inst Oceanol, Moscow, Russia

[2] Russian Acad Sci, Lavrentev Inst Hydrodynam, Siberian Branch, Novosibirsk, Russia

来源：

DOKLADY EARTH SCIENCES | 2017年 / 474卷 / 02期

基金：

俄罗斯科学基金会;

关键词：

ZONE; TRANSPORT;

D O I：

10.1134/S1028334X17060058

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

It has been shown that the total transport of Antarctic Bottom Water (AABW) in the northern fractures (Kane, Cabo Verde, Marathon) are one order of magnitude smaller than in the southern fractures (Vema, Doldrums, Vernadsky). The estimates of AABW transport through this group of fractures based on measurements in 2014 were approximately 0.28 Sv, which is about 25% of the transport through the Vema Fracture Zone. However, the coldest water flows through the Vema Fracture Zone.

引用

页码：653 / 656

页数：4

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