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JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 106, 14975-14984, 2001
Three-dimensional solar radiative transfer in small tropical cumulus fields derived from high-resolution imagery
T. C. Benner, and K. F. Evans
Abstract
Since three-dimensional (3-D) radiative transfer in cloudy atmospheres is too expensive for large-scale atmospheric models,
approximate radiative transfer methods are used. The accuracy of these approximations for a large sample of realistic cloud
fields has not been determined. This study examines 150 fields of small marine tropical cumulus to assess the magnitude of
3-D effects on domain average solar fluxes and to evaluate the accuracy of these approximations in actual cumulus fields.
The cloud fields are derived from Moderate-Resolution Imaging Spectroradiometer Airborne Simulator (MAS) visible and thermal
infrared imagery. Domain average broadband solar fluxes in these fields are simulated with a Monte Carlo radiative transfer
model using four radiative transfer methods: full three-dimensional, the independent pixel approximation (IPA), the tilted IPA,
and the plane-parallel approximation, The average 3-D radiative effects of these cumulus cloud fields are small, with mean
reflected flux errors up to 3 W/m(2) for overhead Sun and less than 1 W/m(2) for the daytime average. The mean errors for
column-absorbed fluxes are less than 0.3 W/m(2) for all Sun angles. The small absolute flux errors are a result of the
average field having small cloud fraction (10%), low cloud optical depth (4.4), and shallow clouds. Some individual fields
have large 3-D absolute reflected flux effects, and the normalized reflected flux errors are significant. The errors correlate
well with the cloud fraction; so it may be possible to make corrections to the approximations.
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