In this study, variability of two oceanic cyclogenesis metrics, tropical cyclone heat potential (TCHP) and effective oceanic layer for cyclogenesis (EOLC) in the Bay of Bengal (BoB) duringNARGIScyclone is investigated.EOLCrepresents the geopotential thickness of near surface stratified layer forms because of the spread of low salinity waters due to fresh water influx from rivers and precipitation. Climatological fields ofTCHPandEOLCreveal thatNARGIStranslated towards the region of higherEOLCas seen in the observations. A maximum daily sea surface cooling of 2 °C is observed along the right and rear side ofNARGIStrack.
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Vissa et al. (2013) studied this question.
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