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Mean field and annual variation of surface flow in the East China Sea as revealed by combining satellite altimeter and drifter data

机译:结合卫星高度计和漂移数据揭示的东海地表水平均场和年变化

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摘要

An analysis of a surface flow field in the East China Sea (ECS) obtained by combining satellite altimeter and drifter data provides comprehensive information of its mean field and annual variation. The Taiwan Warm Current, the onshore Kuroshio intrusion, the Kuroshio, the northeastward Kuroshio branch, the northward current west of Kyushu, the Cheju Warm Current, and the Tsushima Warm Current are regarded as persistent currents. Annual variation is a dominant signal in the ECS and is a major component of the seasonal variation. The contribution of the annual variation to the seasonal variation is estimated as 50% over the ECS, and exceeds 70% for the Kuroshio northeast of Taiwan, the Taiwan Warm Current, the Taiwan Strait Warm Current, the onshore Kuroshio intrusion, the northeastward Kuroshio branch, the northward current west of Kyushu, and the Tsushima Warm Current. The annual variation is characterized by propagation of vorticity anomalies from northeast of the Taiwan Strait and in the Tsushima Strait. The vorticity anomaly from northeast of the Taiwan Strait propagates downstream in the northeastward Kuroshio branch along isobaths of about 100 m on the shelf edge. In contrast, the vorticity anomaly in the Tsushima Strait propagates upstream of the Tsushima Warm Current along isobaths of 100-200 m. The propagation of the vorticity anomalies causes the annual variation with a phase difference in the northeastward Kuroshio branch and the northward current west of Kyushu, and the behavior of the vorticity anomalies can be well explained as a first approximation by a dispersion relation of a quasigeostrophic topographic Rossby wave propagating in a mean flow. Generation of the vorticity anomalies from northeast of the Taiwan Strait and in the Tsushima Strait appears to be closely related to the annual variation of the Kuroshio's current speed northeast of Taiwan and of volume transport through the Tsushima Strait, respectively.
机译:通过结合卫星高度计和漂移数据获得的东中国海(ECS)地表流场分析,可提供有关其平均场和年变化的综合信息。台湾暖流,陆上黑潮侵入,黑潮,东北黑潮分支,九州以西的北流,济州暖流和对马暖流被认为是持续流。年度变化是ECS中的主要信号,并且是季节性变化的主要组成部分。在ECS上,年度变化对季节变化的贡献估计为50%,而对于台湾黑潮东北部,台湾暖流,台湾海峡暖流,陆上黑潮入侵,东北黑潮分支,则超过了70%。 ,九州以西的北流和对马暖流。年变化的特征是从台湾海峡东北部和对马海峡传播涡度异常。台湾海峡东北部的涡度异常沿架子边缘约100 m的等值线向东北黑潮支流下游传播。相比之下,对马海峡的涡度异常沿着100-200 m的等值线在对马暖流的上游传播。涡度异常的传播引起东北向黑潮支流和九州以西的北向电流的年变化,并且具有相位差,并且可以通过准地转地形的色散关系将涡度异常的行为很好地解释为一阶近似。罗斯比波在平均流中传播。来自台湾海峡东北部和对马海峡的涡度异常的产生似乎分别与黑潮目前在台湾东北部的速度和通过对马海峡的运输量的年变化密切相关。

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  • 来源
    《Progress in Oceanography》 |2013年第4期|125-139|共15页
  • 作者单位

    Tohoku Ecosystem-Associated Marine Science, Graduate School of Agricultural Science, Tohoku University, 1-1 Amamiya-machi, Tsutsumidori, Aoba-ku, Sendai-shi,Miyagi 981-8555, Japan;

    Hydrospheric Atmospheric Research Center, Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8601, Japan;

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