“…As one of the key parameters in the vegetation hydrological cycle, canopy storage capacity measures the minimum amount of rainwater required to saturate the vegetation canopy (Dunkerley, 2000; Fathizadeh et al, 2018). There are many factors affecting canopy storage capacity, which can be classified into three categories: (1) meteorological factors, including rainfall amount (Kermavnar & Vilhar, 2017; Liu et al, 2018), intensity (Li et al, 2019), duration (Liu, 1997), temperature, humidity and wind interference (Attarod et al, 2015; Hörmann et al, 1996); (2) vegetation factors, including vegetation types (Xiong et al, 2018; Yan et al, 2021), morphological traits such as leaf area, dry or fresh weights of stem and leaf (Monson et al, 1992; Yan et al, 2021) and canopy characteristics, including coverage, leaf area index (Fleischbein et al, 2005; Kang et al, 2005); and (3) other factors, for instance, disturbance activities (grazing, artificially configured communities) (Lunka & Patil, 2016) and growing seasons (Deguchi et al, 2006; Herbst et al, 2008). Some studies considered the relationships between community structure and canopy storage capacity, but they tended to focus on measuring community structure with direct metrics, for example, aboveground biomass production, leaf area index (LAI), community canopy height and coverage (Deguchi et al, 2006; Holder, 2013; Yu et al, 2012).…”