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Simulation of barotropic and baroclinic tides in the South China Sea

机译:南海正压和斜压潮的模拟

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摘要

The four leading tidal constituents M2, S2, K1 and O1 in the South China Sea are simulated by using POM. The model is forced with tide-generating potential and four leading tidal constituents at the open boundary. In order to simulate more exactly, TOPEX/Poseidon altimeter data are assimilated into the model and the open boundary is optimized. The computed co-tidal charts for M2 and K1 constituents are generally consistent with previous results in this region. The numerical simulation shows that energetic internal tides are generated over the bottom topography such as the Dongsha Islands, the Xisha Islands, the Zhongsha Islands, the Nansha Islands and the Luzon Strait.
机译:利用POM模拟了南海四种主要的潮汐成分M2,S2,K1和O1。该模型被强迫具有潮汐产生潜力,并且在开放边界处具有四个主要的潮汐成分。为了更精确地模拟,将TOPEX / Poseidon高度计数据同化到模型中,并优化了开放边界。计算出的M2和K1成分的共同潮汐图通常与该地区以前的结果一致。数值模拟表明,在东沙群岛,西沙群岛,中沙群岛,南沙群岛和吕宋海峡等海底地形上产生了高能内部潮汐。

著录项

  • 来源
    《海洋学报(英文版)》 |2005年第2期|1-8|共8页
  • 作者

    WU Ziku; LU Xianqing; TIAN Jiwei;

  • 作者单位

    Physical Oceanography Laboratory, Ocean University of China, Qingdao,266003, China;

    Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China;

    Physical Oceanography Laboratory, Ocean University of China, Qingdao,266003,China;

    Physical Oceanography Laboratory, Ocean University of China, Qingdao,266003,China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类
  • 关键词

    tides; South China Sea; TOPEX/Poseidon; assimilation;

    机译:潮汐;南中国海;TOPEX /波塞冬;同化;
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