“…In comparison with herbaceous plants, trees have deeper rooting depth (Canadell et al., 1996), and soil water can be redistributed from wet deep layers to dry surface layers through their root system by hydraulic lift (Prieto, Armas, & Pugnaire, 2012). Therefore, R s in forests may be more buffered from drought than that in grasslands (Davidson, Nepstad, Ishida, & Brando, 2008; Wang, Huang, & Hu, 2020). In addition, fine‐textured soils with good water holding capacity in most forests could weaken the effect of water stress from precipitation reduction on microbial and root activities (Liu, Liu, et al, 2016; Shi, Cheng, Liu, & Jiang, 2005), leading to neutral (Brando et al., 2008; Davidson, Ishida, & Nepstad, 2004; Davidson et al., 2008) or even positive (Cleveland, Wieder, Reed, & Townsend, 2010; Liu, Liu, et al, 2016) responses of R s to drought.…”