Change in the intensity of low-salinity water inflow from the Bay of Bengal into the Eastern Arabian Sea from the Last Glacial Maximum to the Holocene: Implications for monsoon variations
DRS at CSIR-National Institute of Oceanography
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Title |
Change in the intensity of low-salinity water inflow from the Bay of Bengal into the Eastern Arabian Sea from the Last Glacial Maximum to the Holocene: Implications for monsoon variations
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Creator |
Mahesh, B.S.
Banakar, V.K. |
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Subject |
palaeoclimatology
monsoons palaeosalinity foraminifera micropalaeontology temporal variations magnesium isotopes calcium isotopes |
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Description |
A 100–400 km wide region of the coastal Eastern Arabian Sea (EAS), off the west-coast of India, is characterized by a low-salinity tongue formed by the inflow of low-salinity surface water from the Bay of Bengal (BoB). This low-salinity tongue is largely driven by the sea level higher in BoB than in the Arabian Sea and by alongshore pressure gradient between southern- and northern-EAS, and is expected to respond to summer monsoon freshwater flux to the bay. Here, we report past variation in the relative intensity of summer- and winter-monsoons based on changes in the north–south salinity gradient within this low-salinity tongue. The salinity gradient is estimated from paired measurement of delta18O and Mg/Ca in Globigerinoides sacculifer extracted from sediment cores collected at northern high-salinity and southern low-salinity locations within this tongue. The Last Glacial Maximum (LGM) to peak-Holocene delta18O and sea surface temperature gradients at both locations are ~ -2‰ and + 2 °C respectively, while the sea surface salinity gradient at northern-EAS is 0.5 psu higher than in the southern-EAS, suggesting distinctly different SSS structure in the LGM-EAS. The north–south surface salinity gradient was also larger by ~ 0.5 psu during the LGM (1.2 psu) as compared to the gradient during the Holocene (0.7 psu). Increased north–south surface salinity gradient during the LGM suggests diminished flow of low-salinity water into the coastal EAS caused by combined effect of decreased freshening of the BoB and reduced seasonal mountain-river discharge into the EAS. Such surface hydrographic conditions in the coastal EAS clearly indicate significantly weakened summer monsoons and strengthened winter monsoons during the LGM.
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Date |
2014-03-05T10:48:06Z
2014-03-05T10:48:06Z 2014 |
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Type |
Journal Article
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Identifier |
Palaeogeography Palaeoclimatology Palaeoecology, vol.397; 2014; 31-37
no http://drs.nio.org/drs/handle/2264/4477 |
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Language |
en
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Relation |
Bioorg_Med_Chem_Lett_24_2863.jpg
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Rights |
An edited version of this paper was published by Elsevier. Copyright [2013] Elsevier
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Publisher |
Elsevier
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