Assessing the impact of mid-Holocene insolation on the atmosphere-ocean system

A sequence of numerical simulations was performed in order to assess the ro le of early- to mid-Holocene orbital forcing on the coupled atmosphere-ocea n system. Results from both an atmosphere-only general circulation model (G CM) forced by specified sea surface temperatures and a coupled atmosphere-o cean GCM consistently suggest a stronger south Asian monsoon and a strength ened Pacific Walker circulation. The latter feature interacts dynamically w ith the equatorial ocean in the coupled model to produce enhanced Pacific u pwelling, a more pronounced cold tongue, and an even stronger monsoon. Resu lts suggest that the climate of the equatorial Pacific was more similar to the La Nina phase of the modern Southern Oscillation rather than the El Nin o phase.