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Abyssal Boundary Current Studies Current Measurements North of the Falkland Plateau January 1986-1987.

机译：深海边界流研究当前测量当前测量福克兰高原北部1986年1月至1987年。

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The data described in this report were collected in support of the program, Abyssal Boundary Current Studies. This program was designed to improve our understanding of the structure and variability of the deep western boundary currents and to estimate their transport of heat and mass. Some of these deep western boundary currents are formed by the northward flow of the Antarctic Bottom Water along the eastern margins of the southern continents and ridges. In particular these data are from the energetic flow of this Bottom Water entering the South Atlantic. The Weddell Sea is an important formation region for the Bottom Water, some of which flows north through the Georgia Basin and into the South Atlantic. Other portions of the newly formed bottom water may flow to the east of the ridge system containing the Falkland Plateau, Ewing Bank, Falkland Ridge, and the Islas Orcadas Rise. At the North-eastern corner of the ridge system the flow (if present) turns west along the ridge system and becomes part of the clock-wise deep circulation in the Argentina Basin.

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Pillsbury, R. D.; Barstow, D.; Bottero, J. M.; Pittock, G.; Root, D. C.;
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年度 1989
页码 1-422
总页数 422
原文格式 PDF
正文语种 eng
中图分类工业技术;
关键词
Ocean currents; Oceanographic data; Bottom waters; Water masses; Salinity; Mooring; Sampling; Temperature; Velocity; Mass transfer; Heat transfer; Ocean circulation; Weddell Sea;

机译：洋流;海洋学数据;底水;水团;盐度;系泊;取样;温度;速度;传质;传热;海洋环流;威德尔海;

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Abyssal Boundary Current Studies Current Measurements North of the Falkland Plateau January 1986-1987.

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