HYDROLOGIC-CYCLE PARAMETERIZATION FOR ENERGY-BALANCE CLIMATE MODELS

The exchange of moisture and heat between the atmosphere and the Earth 's surface fundamentally affect the dynamics and thermodynamics of the climate system. In order to trace moisture flow through the climate s ystem acid examine its impact on climate, a hydrologic cycle and a lan d surface energy balance are incorporated into a coupled climate - the rmodynamic sea ice (CCSI) model. The expanded CCSI model is tested by comparing its climate simulations with available observations and GCM modeling results. In general, the expanded model does a good job in si mulating the large-scale features of the atmospheric circulation and p recipitation in both space and time. The expanded model is used to exa mine the role of the hydrologic cycle in initiating ice sheet growth i n response to changes in atmospheric composition. The results indicate that variations in summer ice melt in response to changes in the land ice albedo, and thus in air temperatures, are more important in deter mining the initiation of ice sheet growth than variations in precipita tion.