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Volume transport of the western boundary current penetrating into a marginal sea

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摘要

The amount of penetration of a western boundary current into a marginal sea which is connected to an open ocean by two narrow straits is estimated from a linear, steady and barotropic theoretical model. In this model the western boundary current in the open ocean is driven by a wind stress imposed at the sea surface. The inflow of the water of the open ocean into the marginal sea is caused by the pressure difference between two straits produced by the wind-driven circulation in the open ocean.

著录项

  • 来源
    《日本海洋学会誌》 |2005年第4期|185-195|共页
  • 作者

    ShinyaMinato; RyujiKimura;

  • 作者单位

    University of Tokyo;

  • 收录信息 美国《科学引文索引》(SCI);
  • 原文格式 PDF
  • 正文语种 英语
  • 中图分类
  • 关键词

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