ATMOSPHERIC THERMAL REGIME EVOLUTION UNDE R CONDITIONS OF PREDICTED ANTHROPOGENIC POLLUTION

Evolution of the atmospheric thermal regime during period from 1985 to 2100 due to antropogenic pollution is simulated. 1D hemisphere averag ed radiative-convective photochemical model is used. An influence of c limatic feedbacks on thermal regime changes is considered. They are th e conservation of relative or absolute atmospheric humidity and positi ve or negative connection between vertical critical gradient of convec tive adjustment gamma and surface temperature gradient DELTAT(s). An i nfluence of surface thermal inertia is accounted for. Changes of surfa ce temperature, its vertical destribution and ozone content are calcul ated.