Fluctuations of continuous soil moisture evaporation under different rainfall conditions during the growing period of the non-monsoon season, the eastern Loess Plateau.

In Canada ( Gibson et al., 2017 ), the quantitative estimation of the evaporation loss of six lakes based on the C-G model indicated that approximately 18% of the lake water evaporated each year and showed a decreasing trend from south to north.

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In the 20–60 cm soil depth layer, a positive correlation was observed between regional ET 0 and regional soil moisture evaporation loss, and the influence of regional T variability on soil moisture evaporation loss showed an increasing trend.

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