Relationship between Evapotranspiration and Land Surface Temperature under Energy- and Water-Limited Conditions in Dry and Cold Climates

Figure 3

Comparison of simulated and observed soil water content at the depths of 0.5m, 1m, 1.5m, and 2m, respectively. A linear analysis was conducted for each comparison, where is the coefficient of determination and MAE is the mean absolute error.

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