Antarctic Bottom Water Flow through the Eastern Part of the Philip Passage in the Weddell Sea

被引：3

作者：

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

Frey, D., I ^{[1
]}

Tarakanov, R. Yu ^{[1
]}

机构：

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

来源：

OCEANOLOGY | 2020年 / 60卷 / 05期

基金：

俄罗斯科学基金会; 俄罗斯基础研究基金会;

关键词：

Antarctic Bottom Water; Weddell Sea; Philip Passage; Scotia Sea; currents;

D O I：

10.1134/S000143702005015X

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

Measurements of currents and Antarctic Bottom Water properties overflowing the sill from the Weddell to the Scotia Sea are described. The bottom water overflows the sill of one of the passages through the South Scotia Ridge (eastern part of the Philip Passage approximately at 48 degrees W). A weak flow of Weddell Sea Deep Water to the north was found. The northward flow was recorded only in the western part of the passage, which is 14 km wide. The velocity of the flow is 4 cm/s; the bottom water transport is 0.1-0.2 Sv.

引用

页码：589 / 592

页数：4

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