Parameterizations for Cloud Overlapping and Shortwave Single-Scattering Properties for Use in General Circulation and Cloud Ensemble Models

Abstract Parameterizations for cloud single-scattering properties and the scaling of optical thickness in a partial cloudiness condition have been developed for use in atmospheric models. Cloud optical properties are parameterized for four broad bands in the solar (or shortwave) spectrum; one in the ultraviolet and visible region and three in the infrared region. The extinction coefficient, single-scattering albedo, and asymmetry factor are parameterized separately for ice and water clouds. Based on high spectral-resolution calculations, the effective single-scattering coalbedo of a broad band is determined such that errors in the fluxes at the top of the atmosphere and at the surface are minimized. This parameterization introduces errors of a few percent in the absorption of shortwave radiation in the atmosphere and at the surface. Scaling of the optical thickness is based on the maximum-random cloud-overlapping approximation. The atmosphere is divided into three height groups separated approximately by ...

[1]  J. Joseph,et al.  The delta-Eddington approximation for radiative flux transfer , 1976 .

[2]  Knut Stamnes,et al.  Radiative Energy Budget in the Cloudy and Hazy Arctic , 1989 .

[3]  Yongxiang Hu,et al.  An Accurate Parameterization of the Radiative Properties of Water Clouds Suitable for Use in Climate Models , 1993 .

[4]  Harshvardhan,et al.  Parameterization of Solar Near-Infrared Radiative Properties of Cloudy Layers , 1996 .

[5]  Kyu-Tae Lee,et al.  Parameterizations for the Absorption of Solar Radiation by Water Vapor and Ozone , 1996 .

[6]  A. Slingo,et al.  On the shortwave radiative properties of stratiform water clouds , 1982 .

[7]  J. Hansen,et al.  A parameterization for the absorption of solar radiation in the earth's atmosphere , 1974 .

[8]  James J. Hack,et al.  The simulated Earth radiation budget of the National Center for Atmospheric Research community climate model CCM2 and comparisons with the Earth Radiation Budget Experiment (ERBE) , 1994 .

[9]  V. Ramaswamy,et al.  A study of broadband parameterizations of the solar radiative interactions with water vapor and water drops , 1992 .

[10]  Richard B. Rood,et al.  An assimilated dataset for Earth science applications , 1993 .

[11]  W. C. Chao,et al.  Dependence of rainfall on vegetation: theoretical considerations, simulation experiments, observations, and inferences from simulated atmospheric soundings , 1993 .

[12]  K. Liou,et al.  Light scattering by hexagonal ice crystals: comparison of finite-difference time domain and geometric optics models , 1995 .

[13]  A. Slingo A GCM Parameterization for the Shortwave Radiative Properties of Water Clouds , 1989 .

[14]  Robert F. Cahalan,et al.  The albedo of fractal stratocumulus clouds , 1994 .

[15]  Harshvardhan,et al.  Comments on ``The Parameterization of Radiation for Numerical Weather Prediction and Climate Models'' , 1985 .

[16]  Louis Kouvaris,et al.  Calculations of transmission functions in the infrared CO2 and O3 bands , 1991 .

[17]  L. J. Cox Optical Properties of the Atmosphere , 1979 .

[18]  Q. Fu An Accurate Parameterization of the Infrared Radiative Properties of Cirrus Clouds for Climate Models , 1996 .

[19]  M. Chou,et al.  Parameterizations for the Absorption of Solar Radiation by O2 and CO2 with Application to Climate Studies , 1990 .

[20]  C. Sagan,et al.  Anisotropic nonconservative scattering and the clouds of Venus , 1967 .