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Westward intensification in marginal seas

机译：边缘海向西集约化

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摘要

An idealized model was used to examine why the strong western boundary current (WBC) is observed in the South China Sea (SCS) but not in the Gulf of Mexico (GOM) and Japan/East Sea (JES). Results suggested that the stronger WBC in the SCS is mainly attributed to the direct contribution of the inflow and the strong monsoon. Although the Gulf Stream transports a large amount of water into the GOM, the passage in the southeast corner guides the inflow out of the gulf and inhibits the inflow from intensifying the WBC. Meanwhile, the wind stress in the GOM is weakest among the three marginal seas. The meridional ocean ridge and the particular layout of the continental slope of JES prevent the whole basin from participating in the westward intensification. Besides, the throughflow has adverse effects on the formulation of WBC in JES. The variation of Coriolis parameter with latitude leads to the westward intensification in marginal seas. However, a strong WBC cannot be observed in the absence of reasonable collocation of wind, inflow, and topography.
机译：使用理想化模型检查为什么在南中国海（SCS）而不是在墨西哥湾（GOM）和日本/东海（JES）中观察到强西部边界流（WBC）。结果表明，南海的白细胞增强主要归因于流入量和季风的直接贡献。尽管墨西哥湾流将大量的水输送到GOM中，但东南角的通道将流入的水引导出海湾，并抑制了流入水的白化。同时，在三个边缘海中，GOM中的风应力最弱。子午线海脊和JES大陆斜坡的特殊布局阻止了整个盆地参与向西集约化。此外，通流对JES中白细胞的形成有不利影响。科里奥利参数随纬度的变化导致边缘海域向西加剧。但是，在没有合理配置风，入流和地形的情况下，无法观察到强大的白细胞。

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  • 来源
    《Ocean Dynamics》 |2014年第3期|337-345|共9页
  • 作者

    Gengxin Chen; Huijie Xue;

  • 作者单位

    State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, 164 West Xingang Road, Guangzhou 510301, China;

    State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, 164 West Xingang Road, Guangzhou 510301, China,School of Marine Sciences, University of Maine, Orono, ME, USA;

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  • 正文语种 eng
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  • 关键词

    Western boundary current; South China Sea; Gulf of Mexico; Japan/East Sea; Inflow; Topography;

    机译：西部边界流;南中国海;墨西哥湾;日本/东海;流入;地形;

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