HIGHLIGHTS
SUMMARY
Latent heat flux (LE), as the energy expression of Evapotranspiration (ET), is an important link and key component of surface water heat transfer, hydrologic prediction, and hydrological cycle. Based on the EC observation data of the HiWATER test, this study discussed and analyzed the characteristics of evapotranspiration and the impact of various drivers on LE fluxes under different underlying surface types. Studies have shown that different conditions of dry (dune, desert, Gobi) and wet (vegetable land, corn land, wetland) underlying surface, latent heat flux distribution and intradernal variation trend are different, and vegetation cover . . .
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