A STOCHASTIC-MODEL OF GLOBAL ATMOSPHERIC RESPONSE TO ENHANCED GREENHOUSE WARMING WITH CLOUD FEEDBACK

An atmosphere-ocean climate box model is used to examine the influence of cloud feedback on the change in the climate system's variability i n response to enhanced greenhouse warming. The model consists of three nonlinear stochastic differential equations that are simplified forms of the first law of thermodynamics for the atmosphere and ocean and t he continuity equation for the atmospheric component of the hydrologic al cycle. The model is driven by random fluctuations in the mean evapo rative flux, which is routed and distributed among the components of t he system through the fluxes of energy and moisture. The model suggest s that cloud feedback can lead to the occurrence of two climatic regim es into which the present climate may evolve as a result of an enhance d greenhouse warming. In the first regime, the mean values of the mode l parameters, such as temperature, precipitation and cloudiness, as we ll as the amplitude and timescale of their fluctuations all increase m oderately. In the second regime these mean values increase substantial ly, and the amplitude and timescale of their fluctuations rise sharply . The model also predicts the existence of climatic hysteresis; that i s, for the climate system to return from either of these regimes back to the present regime, a substantial decrease in the long-wave forcing is required. (C) 1998 Elsevier Science B.V. All rights reserved.