“…The Kelvin‐Helmholtz (KH) instability is driven by a large sheared flow (Chandrasekhar, 1961), which is an important physical mechanism for the viscous‐like interaction between the Earth's magnetosphere (MSP) and the solar wind (SW) (Axford, 1964; Axford & Hines, 1961). There are lots of in‐situ observation events during both north‐ and southward interplanetary magnetic field (IMF) conditions at low‐latitudes (Blasl et al., 2022; Eriksson, Lavraud, et al., 2016; Henry et al., 2017; Hwang et al., 2011; Kavosi et al., 2023; Li et al., 2013, 2016, 2023; Rice et al., 2022; Wilder et al., 2023; Yan et al., 2014, 2022), as well as at high latitudes with IMF mostly along the dawn or dusk direction (Hwang et al., 2012; Ma et al., 2016; Nykyri et al., 2021). Kavosi and Raeder (2015) shows that for Earth's magnetopause, KH waves occur about 19% of the time.…”