“…DFs are tangential discontinuity with typical thickness comparable to the ion inertial length (e.g., Fu et al., 2012b; Xu et al., 2018) and separate the hot and tenuous plasma from the ambient cold and dense plasma in the magnetotail (e.g., Fu et al., 2012a, 2012b, Fu, Cao, et al., 2013; Runov et al., 2009; Sergeev et al., 2009; Sitnov et al., 2009; Xu et al., 2019). Consequently, the strong gradient of fields and particles at the DFs provide free energy source for the excitement and development of various types of instabilities, such as magnetohydrodynamic (MHD) interchange instabilities (ICI) at MHD scale (e.g., Guzdar et al., 2010; Lapenta & Bettarini, 2011), kinetic interchange instabilities at ion/subβion scales (e.g., Lin et al., 2014; Pritchett & Coroniti, 2010, 2013; Pritchett & Lu, 2018; Pritchett et al., 2014), anisotropy instabilities (e.g., Fu, Cao, Cully, et al., 2014; Fu, Cao, Zhima, et al., 2014; Fu, Chen, et al., 2020; Grigorenko et al., 2020; Guo et al., 2021; Huang et al., 2012; Khotyaintsev et al., 2011; Liu et al., 2017; Zhou et al., 2014), streaming instabilities (e.g., Hwang et al., 2014; Liu, Vaivads, 2019; Yang et al., 2017), and lower hybrid drift instabilities (e.g., Divin et al., 2015; Khotyaintsev et al., 2011; Liu, Fu, Vaivads, 2018; Pan et al., 2018). The PIC simulations shows that the kinetic ICI at DF can lead to the interpenetration of the hot and tenuous plasma and ambient cold and dense plasma and cause the planar surface of DF to become rippled, resulting in perturbations of the magnetic field, density, and electron flow at the front (Pritchett & Coroniti, 2010, Pritchett et al., 2014; Shustov et al., 2019).…”