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Three-dimensional global distributions of longwave radiative cooling for the summer of 1988 and the winter of 1989 are generated from radiative transfer calculations using European Centre for Medium-Range Weather Forecasts temperature and humidity profiles and International Satellite Cloud Climatology Project cloudiness as inputs. By adding the cooling of the clear atmosphere to the total radiative heating, cloud-induced atmospheric radiative heating has been obtained. Emphasis is placed on thedoi:10.1175/1520-0469(1999)056<2657:ciirha>2.0.co;2 fatcat:2hswrqe5wfckjnxfkkofsnuvvu