Transpiration and photosynthesis are closely linked by stomata in terrestrial ecosystems (Jarvis & Daives, 1998;Jones, 1998;Medlyn et al., 2011). The linear relationship between carbon and water is further enhanced by coupling the vapor pressure deficit (VPD) (Beer et al., 2009;S. Zhou et al., 2017). However, the regulation of transpiration is not solely dependent on stomatal conductance but also on environmental conditions, such as radiation, VPD, temperature, and soil water content (SWC) (Jarvis & Mcnaughton, 1986). Recent studies using splitroot experiments and root pressure-chamber investigations have shown that soil water status is a critical factor of transpiration (Comstock, 2002;Hayat et al., 2019;Locke & Ort, 2014). The drying of soil water is consistent with the widespread occurrence of climate drought (Berg et al., 2017), especially in semi-arid and semi-humid climate regions (Cheng & Huang, 2016). Decreased soil moisture controls atmospheric circulation and moisture transport in arid regions (S.