Physical aspects of the greenhouse effect and global warming

According to the simplest model of the earth's radiative balance, global wa rming will occur with certainty as humankind increases its production and c onsumption of nonsolar energy. This prediction is revisited, using a broade r model that allows the greenhouse effect to be considered. The new model p redicts a global warming of Delta T-E =(114 K)epsilon, where epsilon is the rate of surface energy release in units of the average incident solar radi ation, 342 W m(-2), and Delta T-E is the average temperature rise at the ea rth's surface. Present values of these quantities, excluding geothermal sou rces, are epsilon = 0.69 x 10(-4) and Delta T-E = 7.9 mK. The model assigns a small number of optical parameters to the atmosphere and surface and qua lifies the simple warming prediction: It is rigorous only if parameters oth er than epsilon are unchanged. The model is not complex and should serve as an aid to an elementary understanding of global warming. (C) 1999 American Association of Physics Teachers.