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A Quantitative Assessment of the Arabian Sea Sediment Record Using GCM Simulated Upwelling

Published online by Cambridge University Press:  20 January 2017

Grant R. Bigg
Affiliation:
School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, United Kingdom
Dongxiang Jiang
Affiliation:
School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, United Kingdom
John F. B. Mitchell
Affiliation:
Meteorological Office, London Road, Bracknell Berks RG12 2SZ, United Kingdom

Abstract

A general circulation model (GCM) of the ocean is used to study the effects of changes in the monsoon winds of present day and 9000 yr B.P. on the upwelling in the Arabian Sea. The vertical transport from the ocean GCM is used as a measure of upwelling strength to assess the relative abundance of Globigerina bulloides at present and 9000 yr B.P., during the climatic optimum. The high abundance of G. bulloides at 9000 yr B.P. is probably a result of a doubling of the vertical transport at that time.

Type
Research Article
Copyright
University of Washington

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References

Bigg, G.R. Jiang, D. Mitchell, J.F.B. Preliminary results from a general circulation model of the past and present Indian Ocean Ocean Modelling 86 1989 5 8 Google Scholar
Cox, M.D. A Primitive Equation, 3-Dimensional Model of the Ocean GFDL Ocean Group Technical Report No. 1 1984 Google Scholar
Kutzbach, J.E. Guetter, P.J. The sensitivity of monsoon climates to orbital parameter changes for 9000 years BP: Experiments with the NCAR general circulation model Berger, A.L. et al. Milankovitch and Climate 1984 801 820 Google Scholar
Levitus, S. Climatological Atlas of the World Ocean NOAA Prof. Paper No. 13 1982 U.S. Govt. Printing Office Google Scholar
Luther, M.E. O'Brien, J.J. Prell, W.L. Variability in upwelling fields in the northwestern Indian Ocean. 1. Model experiments for the past 18,000 years Paleoceanography 5 1990 433 445 Google Scholar
Mitchell, J.F.B. Grahame, N.S. Needham, K.J. Climate simulation for 9000 years before present: Seasonal variations and effect of the Laurentide ice sheet Journal of Geophysical Research 93 1988 8283 8303 Google Scholar
Pacanowski, R. Philander, S.G.H. Parameterisation of vertical mixing in numerical models of tropical oceans Journal of Physical Oceanography 11 1981 1443 1451 Google Scholar
Prell, W.L. Glacial/interglacial variability of monsoonal upwelling: Western Arabian Sea International Conference: Evolution of Planetary Atmospheres and Climatology of the Earth 1978 Centre National d'Etudes Spatiales Nice, France 149 156 Google Scholar
Prell, W.L. Monsoonal climate of the Arabian Sea during the late Quaternary: A response of changing solar radiation Berger, A.L. et al. Milankovitch and Climate 1984 349 366 Google Scholar
Prell, W.L. Campo, E.V. Coherent response of Arabian Sea upwelling and pollen transport to late Quaternary monsoonal winds Nature 323 1986 526 528 Google Scholar
Prell, W.L. Curry, W.B. Faunal and isotopic indices of monsoonal upwelling: Western Arabian Sea Oceanologica Acta 4 1981 91 98 Google Scholar
Prell, W.L. Kutzbach, J.E. Monsoon variability over the past 150,000 years Journal of Geophysical Research 92 1987 8411 8425 Google Scholar
Zubakov, V.A. Borzenkova, I.I. Global Palaeoclimate of the Late Cenozoic 1990 Elsevier Amsterdam 456 Google Scholar