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Relating surface backscatter response from TRMM precipitation radar to soil moisture: results over a semi arid region

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Figure

Fig. 1. Backscatter map of the Lower Colorado River Basin show-latitudes and 107not covered by TRMM satellite
Fig. 2. Backscatter incidence angle dependence for three vegetation densities (dense, moderate, and low) and three soil water content values,i.e., (a) 15–16%, (b) 19–21%, and (c) 24–26%.
Table 1. List of model parameters of Eq. (2) using VIC soil watercontent for three vegetation densities.
Fig. 5. Images of model parameters (a) A, (b) B, (c) µndvi, (d) N, (e) D, (f) C, and (g) µs
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