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percolation zone or melted snow; on the gentle elevated surface below it, mixed scattering is found,
like dominance of volume scattering, less surface, and double- bounce scattering (see Figure 11.5).
And in the ablation zone of both study areas, a mixed type of scattering is analyzed throughout the
surface, where high volume scattering is seen because of debris/ moraines, double- bounce because
of crevasses and moraines, and much less surface scattering due to the presence of ice in the zone
(see Figure 11.6). Similarly, Freeman– Durden shows quite similar result to H- A- α decompos-
ition, yet the results for the decomposition was not satisfactory; where pixel of H- A- ...