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Detailed Reference Information |
Delaygue, G., Bard, E., Rollion, C., Jouzel, J., Stiévenard, M., Duplessy, J. and Ganssen, G. (2001). Oxygen isotope/salinity relationship in the northern Indian Ocean. Journal of Geophysical Research 106: doi: 10.1029/1999JC000061. issn: 0148-0227. |
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We analyze the surface Δ18O-salinity relationships of the Bay of Bengal and the Arabian Sea, in the northern Indian Ocean, known for their contrasting hydrological conditions. New measurements of these tracers show a very low Δ18O-salinity slope associated with the strong dilution in the Bay of Bengal, but a slope more typical of this latitude in the Arabian Sea. Although this region is marked by a complex monsoonal regime, numerical modeling using a box model and a general circulation model is able to capture the Δ18O-salinity slope and its geographical variation. Both models clearly show that the low Δ18O-salinity slope is due to the evaporation-minus-precipitation balance, with an important contribution of the continental runoff in the Bay of Bengal. Although the low value of these slopes (~0.25) makes past salinity reconstructions uncertain, insight into the Last Glacial Maximum conditions shows a probable stability of these slopes and limited error on paleosalinity. ¿ 2001 American Geophysical Union |
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Abstract |
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Keywords
Meteorology and Atmospheric Dynamics, Ocean/atmosphere interactions (0312, 4504), Meteorology and Atmospheric Dynamics, Paleoclimatology, Oceanography, Biological and Chemical, Stable isotopes, Information Related to Geographic Region, Indian Ocean |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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