Hydrography of the eastern Arabian Sea during summer monsoon 2002
DRS at CSIR-National Institute of Oceanography
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Title |
Hydrography of the eastern Arabian Sea during summer monsoon 2002
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Creator |
Shankar, D.
Shenoi, S.S.C. Nayak, R.K. Vinayachandran, P.N. Nampoothiri, G.S. Almeida, A.M. Michael, G.S. RameshKumar, M.R. Sundar, D. Sreejith, O.P. |
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Subject |
Barrier layer
CTD time series Red Sea Water Persian Gulf Water Water masses |
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Description |
Hydrographic observations in the eastern Arabian Sea (EAS) during summer monsoon 2002 (during the first phase of the Arabian Sea Monsoon Experiment (ARMEX)) include two approximately fortnight-long CTD time series. A barrier layer was observed on occasions during the two time series. These ephemeral barrier layers were caused by in situ rainfall, and by advection of low-salinity (high-salinity) waters at the surface (below the surface mixed layer). These barrier layers were advected away from the source region by the West India Coastal Current and had no discernible effect on the sea surface temperature. The three high-salinity water masses, the Arabian Sea High Salinity Water (ASHSW), Persian Gulf Water (PGW), and Red Sea Water (RSW), and the Arabian Sea Salinity Minimum also exhibited intermittency: they appeared and disappeared during the time series. The concentration of the ASHSW, PGW, and RSW decreased equatorward, and that of the RSW also decreased offshore. The observations suggest that the RSW is advected equatorward along the continental slope off the Indian west coast.
Department of Science and Technology, Department of Ocean Development |
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Date |
2006-03-22T10:20:06Z
2006-03-22T10:20:06Z 2005 |
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Type |
Journal Article
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Identifier |
Journal of Earth System Science, vol. 114(5), 459-474
http://drs.nio.org/drs/handle/2264/14 |
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Language |
en
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Rights |
Copyright with Publisher
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Format |
6430630 bytes
application/pdf |
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Publisher |
Indian Academy of Sciences
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