A radiative transfer model for surface radiation budget studies

Abstract

A high resolution spectral radiative transfer model of the troposphere for computing downwelling radiance and flux density at the surface in the 5–200 μm region has been developed. The model is fast and accurate and takes into consideration all major and minor constituents active in this region, namely, water vapor, carbon dioxide, ozone, nitrous oxide, and methane. It uses the quasi-random band model of absorption for computing atmospheric transmittances due to various bands. Continuum absorption by water vapor in the 8–14 μm region has also been taken into account.The model has been used to examine the sensitivity of downwelling flux to variations of surface water vapor pressure (or surface relative humidity), water vapor scale-height and concentrations of other gaseous constituents of the atmosphere. In addition, sensitivity to changes in a number of cloud parameters, namely, fractional cloud cover, cloud hieght, and high-cloud emissivity, has also been examined. Results obtained with the present model compare well with those from other empirical and semi-empirical correlations. The present work demonstrates, for the first time, the feasibility of using a high-resolution narrow-band model for computing this flux for a meteorological application.