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Waves in Gulf of Mannar and Palk Bay around Dhanushkodi, Tamil Nadu, India

机译:印度泰米尔纳德邦Dhanushkodi附近的Mannar海湾和Palk湾海浪

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摘要

Surface wave characteristics around Dhanushkodi are studied based on the measured data in the Gulf of Mannar and in the Palk Bay. Wave spectra are mainly double-peaked in the Gulf of Mannar and single-peaked in the Palk Bay. High waves (maximum wave height up to 5.4 m) are observed in the Gulf of Mannar compared to the Palk Bay (maximum wave height is 3.6 m). Wave heights are more in the Gulf of Mannar during the southwest monsoon period and the waves are from south-southwest. In the Palk Bay, high waves are found during the northeast monsoon period. Swells dominate the Gulf of Mannar, except during the southwest monsoon period, whereas wind seas exist in the Palk Bay as distant swells cannot reach the bay due to the protection by Indian peninsula and northern extremity of Sri Lanka. Influence of cyclone Laila is observed during the study period in both the Gulf of Mannar and the Palk Bay.
机译:基于在马纳尔湾和帕克湾的实测数据,研究了达纳什科迪周围的表面波特征。波谱主要在马纳那湾为双峰,在波克湾为单峰。与帕克湾(最大波高为3.6 m)相比,在马纳尔湾观察到高波(最大波高至5.4 m)。西南季风期间,马纳那湾的海浪高度更高,海浪来自西南偏南。在帕克湾(Palk Bay),在东北季风时期发现高风。除西南季风时期外,隆起主导着马纳尔湾,而帕克湾则存在风浪,因为印度半岛和斯里兰卡北端的保护使遥远的隆起无法到达海湾。在研究期间,在马纳尔湾和帕克湾均观察到了莱拉飓风的影响。

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