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基于高频地波雷达观测的大亚湾附近海域余流季节变化特征分析

Analysis of the seasonal variation of the residual currents by HF Surface Wave Radar data in adjacent waters of Daya Bay

  • 摘要: 基于大亚湾附近海域高频地波雷达的长期海流观测资料,利用T_tide工具包进行调和分析得到该海域余流季节变化特征。分析结果显示:大亚湾附近海域余流的变化特征主要呈冬、夏两种形态,其变化过程与季风的变化同步。其中,冬季形态从10月到次年3月,流向为SW向,流速可达30 cm/s以上;夏季形态仅在5—8月间出现,流向为NE向,流速可达23 cm/s。大亚湾附近海域的余流分布特征不仅与海表面风场变化相关,而且与海底地形也存在显著相关关系。此外,粤东沿岸流与珠江冲淡水对大亚湾附近海域余流空间分布具有调控作用。

     

    Abstract: The seasonal variation of residual currents in adjacent waters of Daya Bay was analyzed based on the longterm current data observed by HF Radar with T_tide toolkit. The results showed that the variation of residual current in adjacent waters of Daya Bay was mainly the types of winter and summer and it changed synchronously with monsoon. The residual current flowed southwest in winter, which lasted from October to March of the next year, and the current velocity had reached more than 30 cm/s. While the residual current flowed northeast in summer, which lasted only from May to August, with velocity up to 23 cm/s. The seasonal variation of residual currents was not only correlated with wind, but also significantly correlated with the seabed topography. Besides, the east Guangdong coastal current and the Pearl River diluent water had regulating effect on the spatial distribution of residual current in adjacent waters of Daya Bay.

     

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