Abstract
Given the pronounced warming in the Indian Ocean sea surface temperature (SST) during the second half of the twentieth century and the empirical relationship between the Indian Ocean SST and Sahel summer precipitation, we investigate the mechanisms underlying this relationship using the GFDL atmospheric model AM2.0 to simulate the equilibrium and transient response to the warming of the Indian Ocean. Equatorial wave dynamics, in particular the westward propagating equatorial Rossby waves, communicates the signal of tropospheric warming and stabilization from the Indian Ocean to the African continent. The stabilization associated with the Rossby wave front acts to suppress the convection. Feedbacks with local precipitation and depletion of moisture amplify the dynamically induced subsidence. While this stabilization mechanism is expected to operate in climate change response, the future prospects for the Sahelian climate under global warming are complicated by the intricate sensitivities to the SSTs from different ocean basins and to the direct radiative forcing of greenhouse gases.
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Acknowledgements
I like to first acknowledge Drs. I. M. Held and T. L. Delworth for their mentorship during my visit at GFDL when the reported work was carried out. I am indebted to A. Giannini and M. Biasutti for providing the station based Sahel rainfall index and data from the NSSIP1 simulations and their helpful comments during the formative stage of the paper. I would like to express my appreciation to M. Hoerling and another anonymous reviewer for their perceptive review, which helps improve substantially the manuscript. I also thank G. Meehl and A. Sealy for their encouragement and conducting the NCAR internal review. I acknowledge the Climate Research Unit at University of East Anglia for providing the gridded land precipitation data set. X. Jiang provided the linearized dry GCM for the experiments on the dry response to a prescribed equatorial heating. J. Lu is supported by the Advance Study Program (ASP) at NCAR.
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Lu, J. The dynamics of the Indian Ocean sea surface temperature forcing of Sahel drought. Clim Dyn 33, 445–460 (2009). https://doi.org/10.1007/s00382-009-0596-6
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DOI: https://doi.org/10.1007/s00382-009-0596-6