Show simple item record

dc.contributor.authorMorwal, S.B.
dc.contributor.authorNagar, S.G.
dc.contributor.authorMurty, V.S.N.
dc.contributor.authorSeetaramayya, P.
dc.date.accessioned2006-11-20T11:40:01Z
dc.date.available2006-11-20T11:40:01Z
dc.date.issued2006
dc.identifier.citationJournal of Earth System Science, vol.115(5), 587-599p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/499
dc.description.abstractDuring the period 12–16 June 1996 a tropical cyclonic storm formed over the southwest Bay of Bengal and moved in a north–northeasterly direction. The thermodynamic characteristics of this system are investigated by utilizing the surface and upper air observations collected onboard ORV Sagar Kanya over the Bay of Bengal region. The response of the cyclonic storm is clearly evident from the ship observations when the ship was within the distance of 600–800 km from the cyclonic storm. This study explores why (1) the whole atmosphere from surface to 500 hPa had become warm and moist during the cyclonic storm period as compared to before and after the formation of this system and (2) the lower layer of the atmosphere had become stable during the formative stage of the cyclonic storm.
dc.format.extent1303814 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen
dc.publisherIndian Academy of Sciences
dc.rightsFull-text of the paper hosted with the permission from Publisher.
dc.subjecttropical cyclonic storm
dc.subjectBay of Bengal
dc.titleMarine boundary layer characteristics during a cyclonic storm over the Bay of Bengal
dc.typeJournal Article


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record