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dc.contributor.authorSumesh, K.G.
dc.contributor.authorRameshKumar, M.R.
dc.date.accessioned2013-09-06T07:41:33Z
dc.date.available2013-09-06T07:41:33Z
dc.date.issued2013
dc.identifier.citationNatural Hazards, vol.68(2); 2013; 1057-1074
dc.identifier.otherno
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/4361
dc.description.abstractTropical cyclones are the most hazardous weather systems, which form over warm ocean waters. The frequencies of tropical cyclones show variabilities over all the oceanic basins, during the El-Nino and El-Nino Modoki years. Recent studies have shown significant impact of air–sea interaction processes like El-Nino and El-Nino Modoki on the cyclone activity over different ocean basins. The results suggest in most cases, El-Nino events suppress the formation of cyclones over various basins. A recent study indicated that concurrent occurrence of El-Nino Modoki and positive Indian Ocean dipole (IOD) events can generate more cyclones over north-west Pacific. We propose to study the impact of El-Nino Modoki events on the formation of tropical cyclones over north Indian Ocean (NIO). Our present study suggests that the cyclogenesis over the NIO is a complex phenomenon, as it is influenced by several coupled ocean atmospheric phenomena such as El-Nino, El-Nino Modki, IOD and Madden–Julian oscillation
dc.language.isoen
dc.publisherSpringer
dc.relation.requiresNat_Hazards_68_1057.jpg
dc.rightsAn edited version of this paper was published by Springer. This paper is for R & D purpose and Copyright [2013] Springer.
dc.subjectEl Nino phenomena
dc.subjecthurricanes
dc.subjectair-sea interaction
dc.subjectcyclogenesis
dc.titleTropical cyclones over north Indian Ocean during El-Nino Modoki years
dc.typeJournal Article


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