Figures
Figure 1. Difference between grid point maximum snow albedo
(determined by Robinson and Kukla, 1985) and background surface albedo
calculated by the WRF Preprocessing System with input from the WRF
vegetation parameter lookup table. In principle, these values represent
the maximum albedo gradient across a hypothetical local snow line. The
large region of enhanced albedo difference in the center of the
continent represents the Great Plains study area.