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首页> 外文期刊>日本海洋学会誌 >Effects of a marine ridge to western boundary current in a three-dimensional source-sink flow model
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Effects of a marine ridge to western boundary current in a three-dimensional source-sink flow model

机译:海脊对三维源槽流动模型中的西界电流的影响

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摘要

A numerical experiment is made with a three-dimensional source-sink flow model in order to study effects of a marine ridge to the western boundary current. The model represents the Kuroshio current crossing the Izu Ridge which has a submarine narrow passage. It is indicated that most of the surface water of the western boundary current crosses the ridge through the narrow passage. A part of the surface water circulates around a warm eddy formed in an upstream region of the ridge. A water below the thermocline makes a long detour around the ridge and forms a subsurface northward current along the eastern slope of the ridge.
机译:用三维源槽流模型制造数值实验,以便研究海脊对西部边界电流的影响。该模型代表了穿过具有潜艇窄通道的Izu脊的Kuroshio电流。结果表明,西部边界电流的大多数表面水通过窄通道穿过脊。表面水的一部分围绕形成在脊的上游区域的温暖涡流周围。热水下部下方的水在脊周围长时间弯曲,沿着脊的东坡形成落地北电流。

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