dc.contributor.author | Sumesh, K.G. | |
dc.contributor.author | RameshKumar, M.R. | |
dc.date.accessioned | 2013-09-06T07:41:33Z | |
dc.date.available | 2013-09-06T07:41:33Z | |
dc.date.issued | 2013 | |
dc.identifier.citation | Natural Hazards, vol.68(2); 2013; 1057-1074 | |
dc.identifier.other | no | |
dc.identifier.uri | http://drs.nio.org/drs/handle/2264/4361 | |
dc.description.abstract | Tropical 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.iso | en | |
dc.publisher | Springer | |
dc.relation.requires | Nat_Hazards_68_1057.jpg | |
dc.rights | An edited version of this paper was published by Springer. This paper is for R & D purpose and Copyright [2013] Springer. | |
dc.subject | El Nino phenomena | |
dc.subject | hurricanes | |
dc.subject | air-sea interaction | |
dc.subject | cyclogenesis | |
dc.title | Tropical cyclones over north Indian Ocean during El-Nino Modoki years | |
dc.type | Journal Article | |