Estimation of Groundwater Evapotranspiration Using Diurnal Groundwater Level Fluctuations under Three Vegetation Covers at the Hinterland of the Badain Jaran Desert

<div>Estimated groundwater evapotranspiration (ET<sub>G</sub>) and interpolated evapotranspiration rate (ET<sub>C</sub>) based jointly on the white and Mazur’s methods and potential evapotranspiration (PET) at the observation site G6.</div>

Advances in Meteorology

fig8

Figure 8

Figure 8: Estimation of Groundwater Evapotranspiration Using Diurnal Groundwater Level Fluctuations under Three Vegetation Covers at the Hinterland of the Badain Jaran Desert 

Figure 8 | Estimation of Groundwater Evapotranspiration Using Diurnal Groundwater Level Fluctuations under Three Vegetation Covers at the Hinterland of the Badain Jaran Desert 