Wind Speed-Independent Two-Source Energy Balance Model Based on a Theoretical Trapezoidal Relationship between Land Surface Temperature and Fractional Vegetation Cover for Evapotranspiration Estimation

<div>Estimated <i>T</i><sub>c</sub> and <i>T</i><sub>s</sub> from the soil wetness isoline and the two-stage ET with observed two-layer soil moisture at the DM station; the soil moisture in the root zone is the average of 20, 40, and 80 cm based on the research of Wu et al. [<a href="/journals/amete/2020/6364531/#B72">72</a>].</div>

Advances in Meteorology

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Figure 11

Figure 11: Wind Speed-Independent Two-Source Energy Balance Model Based on a Theoretical Trapezoidal Relationship between Land Surface Temperature and Fractional Vegetation Cover for Evapotranspiration Estimation 

Figure 11 | Wind Speed-Independent Two-Source Energy Balance Model Based on a Theoretical Trapezoidal Relationship between Land Surface Temperature and Fractional Vegetation Cover for Evapotranspiration Estimation 