On an upwelling front along the west coast of India during later part of southwest monsoon

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dc.contributor.author Unnikrishnan, A.S.
dc.contributor.author Antony, M.K.
dc.date.accessioned 2009-05-08T12:10:01Z
dc.date.available 2009-05-08T12:10:01Z
dc.date.issued 1992
dc.identifier.citation Physical processes in the Indian Seas. Proc. 1 Convention ISPSO, 1990. Ed. by: Swamy, G.N., 131-135p.
dc.identifier.uri http://drs.nio.org/drs/handle/2264/3098
dc.description.abstract A coastal front, associated with upwelling, is identified from the observed thermal field along the west coast of India during September, 1987. The front, which is seen very clearly upto a depth of about 75 m, has a horizontal gradient of temperature of about 6 degrees C over a width varying between 45 and 70 km. An alongshore temperature section passing through the offshore side of the front shows a north-south slope of the thermocline, which is shallow at the southern side and deep at the northern side. It is speculated from the observed features that upwelling along the west coast of India occurs first at the southern part and the signal gradually propagates towards north
dc.language.iso en
dc.publisher Indian Society for Physical Sciences of the Oceans
dc.rights Copyright [1992]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.title On an upwelling front along the west coast of India during later part of southwest monsoon
dc.type Conference Article


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