A Landsat Thematic Mapper scene over Terre Adélie, Antarctica, is used to estimate the snow grain-size. New calibration coefficients are computed for the TM scene, using sea-water reflectance. Topographic effects are corrected with the visible band TM2. Atmospheric effects are taken into account. The snow theoretical reflectance is calculated with the Wiscombe and Warren (1980) model. Estimated snow grain-sizes are similar to those given in the literature.
No takes yet. Share an insight, caveat, or question.
Bourdelles et al. (1993) studied this question.
Synapse has enriched 4 closely related papers on similar clinical questions. Consider them for comparative context: