加的斯湾地中海潜流的变化

S.A. Thorpe
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引用次数: 65

摘要

1970年3月和1971年3月,在地中海暗流的加的斯湾北侧测量了海流、温度和盐度。观察集中在两个地区。在第一种情况下,潜流与海床分离,虽然与北侧的大陆斜坡接触,但仍以自由射流的形式流动;而在第二种情况下,潜流与海床直接接触,并受海底山谷地形的影响。这些测量表明了暗流的中尺度变化,以及密集的近底水的到达和上覆水的漩涡运动对第一个区域的流动的中断。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Variability of the mediterranean undercurrent in the Gulf of Cadiz

Measurements of currents, temperatures and salinities were made in March 1970 and 1971 on the north side of the Gulf of Cadiz in the Mediterranean undercurrent. Observations were concentrated in two areas. In the first the undercurrent is free from the sea bed and flows as a free jet although in contact with the continental slope on its northerly side, whilst in the second it is in direct contact with the sea bed and influenced by the topography of a submarine valley. These measurements demonstrate the mesoscale variability of the undercurrent, and the interruption of the flow in the first area by the arrival of denser near-bottom water and an eddy-like motion in the overlying water.

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