

Type of Document Dissertation Author Villeneuve, Pierre V. URN etd-2047101569611961 Title A Numerical Study of the Sensitivity of Cloudy-Scene Bidirectional Reflectivity Distribution Functions to Variations in Cloud Parameters Degree PhD Department Mechanical Engineering Advisory Committee
Advisor Name Title Campbell, James B. Jr. Nelson, Douglas J. Scott, Elaine P. Stern, Curtis H. Mahan, James Robert Committee Chair Keywords
- none
Date of Defense 1996-06-28 Availability unrestricted Abstract The goal of this research has been to characterize the sensitivity of the earth's
shortwave bidirectional reflectivity distribution function (BRDF) to variations in
cloud parameters. The BRDF is a remote sensing tool used to predict the flux
reflected from a given earth scene from a satellite-based measurement of the
reflected intensity. The BRDF is necessary in order to account for the anisotropic
nature of the shortwave radiation field. A shortwave atmospheric radiation
Monte-Carlo ray-trace model has been developed as part of this research to predict
the earth-reflected radiation field at the top of the atmosphere. This model was
developed while paying special attention to clouds including realistic
three-dimensional cloud fields characterized by fundamental physical properties.
This model was used to predict the BRDF for various cloud fields where a single
cloud parameter was varied as part of the sensitivity analysis. The results show that
the shortwave BRDF is very sensitive to changes in cloud vertical thickness and
mean cloud size. This sensitivity is also strongly dependent on the direction from
which the scene is observed. In a related analysis, a study was done of the error
associated with using a BRDF from one scene to retrieve fluxes from a second
scene. The model was also used to predict images of cloud fields for comparison
with experimental data from the Rutherford Appleton Laboratories satellite-based
Along Track Scanning Radiometer (ATSR). Finally the output from the radiation
model was integrated with the end-to-end radiative electrothermal model of a
practical earth radiation budget instrument. This integrated model was used to
predict the instrument response to scanning a realistic partly-cloudy earth scene.
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