The spatial patterns of tropical precipitation in the control aquaplanet simulations, its modification by the introduction of land, and its response to climate change vary dramatically between the models, even in this simple setup. We will use recent ideas on the local moist energy balance of the tropical atmosphere to diagnose some of the causes of this diversity. Our goal is to trace intermodel differences in circulation and precipitation to differences in the cloud and clear-sky radiative effects and the gross moist stability, and ultimately to the cloud and convective parameterizations themselves. This will give insight into what determines the monsoons, Walker cells and other zonal-seasonal asymmetries in the tropical atmosphere.
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