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dc.contributor.authorMankad, Bhasha M.-
dc.contributor.authorSharma, Rashmi-
dc.contributor.authorBasu, Sujit-
dc.contributor.authorPal, P. K.-
dc.date.accessioned2014-02-05T09:26:50Z-
dc.date.available2014-02-05T09:26:50Z-
dc.date.issued2014-01-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/26425-
dc.description50-53en_US
dc.description.abstractSatellite and in situ observations in the equatorial Indian Ocean have shown spectral peaks at 30-60 days and at 90 days periods. However, spectral analysis of thermocline variability in this particular ocean basin seems to have escaped the attention of researchers. In this study such an analysis has been carried out using primarily the data from a buoy. Other auxiliary data like satellite observed sea level anomaly and winds have also been used in this study. Further supporting evidence comes from the data generated by a numerical ocean circulation model. This model has been forced by QuikSCAT scatterometer winds and NCEP fluxes. Spectral analysis of current, thermocline depth and sea level anomaly from this model also supports the existence of the mentioned periodicities.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.43(1) [January 2014]en_US
dc.subjectThermocline variabilityen_US
dc.subjectSea levelen_US
dc.subjectEqutorialen_US
dc.subjectSpectral analysisen_US
dc.titleIntraseasonal thermocline variability in the Equatorial Indian Oceanen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.43(01) [January 2014]

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