作者: N. P. Kurian , N. Nirupama , M. Baba , K. V. Thomas
DOI: 10.1007/S11069-008-9260-4
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摘要: Coastal flooding occurs due to storm surges generated by tropical and extra-tropical cyclones on the globe. The meteorological forcing fields for generation of are tangential surface wind stress ocean normal atmospheric pressure gradients associated with weather systems. large scale from is referred as synoptic surge prediction well developed reasonably satisfactory around world. However, coastal also systems, a meso-scale remote forcing. It proposed here that term “Storm surge” be used only refer terminology “Rissaga” For forcing, new “Kallakkadal” proposed.