Premonsoonal water characteristics and cirulation in the east central Arabian sea
DRS at CSIR-National Institute of Oceanography
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Title |
Premonsoonal water characteristics and cirulation in the east central Arabian sea
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Creator |
RameshBabu, V.
Sastry, J.S. Gopalakrishna, V.V. RamaRaju, D.V. |
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Description |
The hydrographic structure in the east central Arabian Sea during premonsoon period undergoes significant temporal change in the thermal field of upper 100 m, wherein temperature rises by about 0.5 degrees C on an average from May to June. The major contribution in increasing the surface layer temperature comes from surface heat exchange processes, while the horizontal advective process tends to remove the heat from the upper layer. The geostrophic flow patterns are similar from May to June in the major part of the study area while in the coastal areas off Goa a southerly current sets in June in response to coastal upwelling.
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Date |
2009-05-12T10:43:04Z
2009-05-12T10:43:04Z 1991 |
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Type |
Journal Article
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Identifier |
Proceedings of the Indian Academy of Sciences (Earth and Planetary Sciences), Vol.100; 55-68p.
http://drs.nio.org/drs/handle/2264/3345 |
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Language |
en
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Rights |
Copyright [1991]. 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.
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Publisher |
Indian Academy of Sciences
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