“…Regarding the meteorological controls on plant water use, many studies have found fairly good linear relationships at the daily scale between transpiration and radiation and vapour pressure deficit ( VPD ), which are two major controlling factors as shown recently, for example, for plants in a desert‐oasis wetland of northwest China (Liu, Zhao, Wen, & Zhang, ), Scots pine in a boreal, humid Scottish catchment (Wang, Tetzlaff, Dick, & Soulsby, ), and tropical montane cloud forest in São Paulo Brazil (Eller, Burgess, & Oliveira, ). However, at the sub‐daily scale (i.e., hourly), the linear relationships between Ec and environmental variables have been shown to be weaker in most studies (Ma et al, ; Tie, Hu, Tian, Guan, & Lin, ; Wang et al, ). It is worth noting that because time lags have been found between transpiration from leaves and sap flow in the xylem, which vary among plant species (Goldstein et al, ; Kume, Komatsu, Kuraji, & Suzuki, ), environmental controls on sub‐daily plant water use are often examined using xylem sap flow or sap flux ( Js ) as a proxy when transpiration from leaves is not directly measured (Aranda, Forner, Cuesta, & Valladares, ).…”