Titlebook: Clouds, Chemistry and Climate; Paul J. Crutzen,Veerabhadran Ramanathan Conference proceedings 1996 Springer-Verlag Berlin Heidelberg 1996

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GCM Studies and Parameterization,st of which are inadequately understood. The spatial scales involved in cloud formation range from tenths of micrometers for cloud condensation nuclei to hundreds of kilometers for large-scale dynamics. Most of these processes cannot be resolved by the current generation of climate models with typic

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The Central Equatorial Pacific Experiment,) are within a narrow range between 300 K and 303 K, and less than 0.01% of the ocean surface has SSTs in excess of 304 K (Figure 1). Furthermore, deep convection is triggered only when SSTs exceed 300 K. In regions of deep convection and warm SST, the reduction of outgoing longwave energy by the at