Abstract

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° 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.

中文翻译：

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南极底部水流过韦德尔海菲利普河道的东部

摘要

描述了水流和南极海底水质从韦德尔溢流到斯科舍海的测量。底部水溢出通过南斯科舍海脊（菲利普河段的东部，大约在48°W）的其中一个通道的窗台。发现北部的韦德尔海深水微弱。仅在通道的西部记录了北流，该通道的宽度为14 km。流速为4 cm / s；底部水的输送量为0.1–0.2 Sv。