“…It controls the SM‐precipitation feedback at continental scale and runoff‐precipitation response at watershed scale. As a result, SM observations are widely used in meteorology, hydrology and climatology (Peng, Loew, Merlin, & Verhoest, 2017; Yin, Hain, Zhan, Dong, & Ek, 2019; Yin, Zhan, Hain, Liu, & Anderson, 2018). The development of ground‐based SM measurement techniques provides an opportunity to obtain SM estimates at different soil depths (Robinson et al, 2008, Dobriyal et al, 2012, Vereecken et al, 2014) with the in situ observations commonly considered as the “truth” to validate satellite and model SM simulations against.…”