“…The earthward transport of mass and magnetic flux, usually accompanied by intermittent coherent structures, such as bursty bulk flows (BBF) (e.g., Angelopoulos et al, 1992; Cao et al, 2006, , 2013) and dipolarization fronts (e.g., Fu, Khotyaintsev, Vaivads, André, & Huang, 2012a, 2012b; Fu, Cao, et al, 2013; Liu et al, 2013; Liu, Fu, Xu, et al, 2018; Liu, Fu, Vaivads, et al, 2018; Nakamura et al, 2002; Runov et al, 2009; Sergeev et al, 2009; Yao et al, 2017), ultimately provides sufficient energy for the auroral substorms (e.g., Angelopoulos et al, 2008; Liu et al, 2014; Liu, Fu, Xu, et al, 2018; Yao et al, 2012). One typical signature associated with such energy transport is the increase of suprathermal (from tens to hundreds of keV) electron flux in the terrestrial magnetotail (e.g., Asano et al, 2010; Kronberg et al, 2017; Pan et al, 2014; Turner et al, 2016), which results from local acceleration at reconnection region (e.g., Chen, Fu, Zhang, et al, ; Drake et al, 2006; Egedal et al, 2010; Hoshino et al, 2001; Huang, Vaivads, et al, 2012; Fu, Xu, et al, 2019; Øieroset et al, 2002; Vaivads et al, 2011; Fu et al, ) and dipolarization fronts (DFs) (e.g., Ashour‐Abdalla et al, 2011; Birn et al, 2014; Duan et al, 2014; Fu et al, 2011; Fu, Khotyaintsev, et al, 2013; Fu, Grigorenko, et al, 2020; Gabrielse et al, 2016; Huang, Zhou, et al, 2012; Khotyaintsev et al, 2011; Liu, Fu, Xu, Wang, et al, 2017; Liu, Fu, Cao, Xu, et al, 2017; Liu, Liu, Xu, et al, 2018; Liu et al, 2019; Lu et al, 2016; Pan et al, 2012; Runov et al, 2013; Wu et al, 201...…”