The solar radiation parameterization (CLIRAD-SW) developed at the Goddard Climate and Radiation Branch for application to atmospheric models are described. It includes the absorption by water vapor, O3, O2, CO2, clouds, and aerosols and the scattering by clouds, aerosols, and gases. Depending upon the nature of absorption, different approaches are applied to different absorbers. In the ultraviolet and visible regions, the spectrum is divided into 8 bands, and single O3 absorption coefficient and Rayleigh scattering coefficient are used for each band. In the infrared, the spectrum is divided into 3 bands, and the k-distribution method is applied for water vapor absorption. The flux reduction due to O2 is derived from a simple function, while the flux reduction due to CO2 is derived from precomputed tables. Cloud single-scattering properties are parameterized, separately for liquid drops and ice, as functions of water amount and effective particle size. A maximum-random approximation is adopted for the overlapping of clouds at different heights. Fluxes are computed using the Delta-Eddington approximation.Chou, Ming-Dah and Suarez, Max J. (Editor)Goddard Space Flight CenterSOLAR RADIATION; ATMOSPHERIC MODELS; EDDINGTON APPROXIMATION; PARAMETERIZATION; ATMOSPHERIC RADIATION; ABSORPTIVITY; RADIANT HEATING; AEROSOLS; OZONE; CARBON DIOXIDE; OXYGEN; RAYLEIGH SCATTERING; SCATTERING COEFFICIENTS; WATER VAPOR; CLOUDS (METEOROLOGY)...