首页|期刊导航|北京大学学报(自然科学版)|基于高频地波雷达观测的海南岛西侧潮流特征及其对台风的响应

基于高频地波雷达观测的海南岛西侧潮流特征及其对台风的响应OA北大核心

Tidal Current Characteristics and Response of Tidal Current to Typhoon on the West Side of Hainan Island by High Frequency Radars

中文摘要英文摘要

基于高频地波雷达观测得到的海南岛西侧海洋表层流场数据,运用调和分析等方法,研究该海域潮流特征及其季节变化规律.结果表明,该海域浅水分潮显著,潮流性质主要为全日潮,其中偏北部分为不规则全日潮,偏南部分为规则全日潮.潮流运动以顺时针往复流为主,南部的最大可能潮流流速大于北部,其中最大可能潮流流速在南部为 1.2~1.8 m/s,北部为 0.25~1 m/s.此外,计算了潮流对台风"小熊"的响应情况,结果表明,台风导致表层潮流强度在短时间内减弱,在台风过境 7天后,潮流强度基本上恢复至台风影响前的状态,与半日潮相比,该现象在全日潮中更明显.

Based on the surface flow field data from high-frequency radar on the west side of Hainan Island,harmonic analysis and some other methods were employed to investigate the tidal current characteristics and their seasonal variations in this region.The results show significant shallow-water tidal features,with the tidal currents predominantly diurnal.The northern part of the study area exhibits irregular diurnal tidal characteristics,while the southern part displays regular diurnal tidal patterns.The tidal current mainly follows a clockwise reciprocating motion,with the maximum potential tidal current velocity being stronger in the south region than that in the north region.Specifically,the maximum possible tidal current velocity is 1.2-1.8 m/s in the south and 0.25-1 m/s in the north.In addition,the impact of Typhoon"Koguma"on the tidal current was also calculated.The results indicate that the typhoon temporarily weakens the surface tidal current intensity,which generally recovers to normal intensity within seven days.Compared with semi-diurnal tides,this phenomenon is more pronounced in diurnal tides.

陈曦;杨凡;韦骏

广西大学海洋学院,南宁 530004国家海洋局珠海海洋环境监测中心中心站,珠海 519000中山大学大气科学学院,南方海洋科学与工程广东省实验室(珠海),珠海 519000

北部湾潮流高频地波雷达台风表层流

Beibu Gulftidal currentHF radartyphoonsurface current

《北京大学学报(自然科学版)》 2025 (1)

53-64,12

南方海洋科学与工程广东省实验室自主项目(SML2020SP009)资助

10.13209/j.0479-8023.2025.007

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