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Estimate soil moisture using trapezoidal relationship between remotely sensed land surface temperature and vegetation index

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Table 2. Correlation coe ffi cients between WDI estimates with surface soil moisture observa- observa-tions.
Fig. 1. The hypothetical trapezoidal shape based on the relation between (T s − T a ) and the fractional vegetation cover (V c ).
Fig. 2. Iterative procedure for calculating T s of the four vertices of T s -VI trapezoid.
Fig. 3. Digital elevation model (DEM) of Walnut Gulch Experimental.
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