A multi-model analysis of the role of the ocean on the African and Indian monsoon during the mid-Holocene


We investigate the role of the ocean feedback on the climate in response to insolation forcing during the mid-Holocene (6,000 year BP) using results from seven coupled ocean–atmosphere general circulation models. We examine how the dipole in late summer seasurface temperature (SST) anomalies in the tropical Atlantic increases the length of the African… (More)

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