Please use this identifier to cite or link to this item: http://nopr.niscair.res.in/handle/123456789/38306
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dc.contributor.authorKumar, K V Sanil-
dc.contributor.authorMadhusoodanan, P-
dc.contributor.authorJoseph, M G-
dc.contributor.authorMathew, Basil-
dc.date.accessioned2016-12-08T09:42:01Z-
dc.date.available2016-12-08T09:42:01Z-
dc.date.issued1991-12-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38306-
dc.description239-243en_US
dc.description.abstractMeteorological parameters at a station (9-degrees-N, 68-degrees-E) in the east central Arabian Sea showed the influence of a severe cyclonic storm that formed east of Sri Lanka in the first week of May 1979. One dimensional forcing functions, such as, free and forced mixing were important for regulating thermal structure in this area during the disturbed days (phase I: 2 to 14 May 1979). But, this was marginal during the calm days (phase II: 25 May to 4 June). The results of the study were utilised to model the mixed layer temperature (MLT) and mixed layer depth (MLD) following Niiler and Kraus (1977). During phase I, simulated and observed MLD and MLT matched fairly well. The differences between the observed and simulated MLT during phase II were attributed to lateral advective cooling.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.20(4) [December 1991]en_US
dc.titleMixed layer variability in east central Arabian Sea during premonsoon season of 1979en_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.20(4) [December 1991]

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