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Advancing the AirMOSS P-Band Radar Root Zone Soil Moisture Retrieval Algorithm via Incorporation of Richards’ Equation

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Figure

Table 1 in this paper), Eq. (12) can be approximated as:
Figure 1. The best fit of Eq. (21) (solid lines) to HYDRUS-1D simulation results (circles) for simultaneous evaporation and drainage in three different soils
Table 1. Average van Genuchten model parameters for the 12 USDA soil textural classes [40] as well as parameters for Eqs
Figure 2. The best fit of Eq. (21) (lines) to into a loam soil with parameters given in HYDRUS-1D simulation results (circles) for a constant-flux (= 1 cm h-1) infiltration process Table 1
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