“…These structures were first identified in the solar wind (Turner et al, 1977), and were subsequently observed frequently in the planetary magnetosheath (e.g., Cattaneo et al, 1998; Balikhin et al, 2009; Tsurutani et al, 2011; Yao ST et al, 2017), in the magnetotail (e.g., Ge YS et al, 2011; Yao ST et al, 2016; Zhang XJ et al, 2017), in the magnetospheric cusp (Shi QQ et al, 2009; Jasinski et al, 2017), and even in the magnetosphere of comets (Russell et al, 1987; Plaschke et al, 2018). They have been identified under various names according to their generation mechanisms and property features, for example, “magnetic dips”, “magnetic decreases”, “mirror modes”, and “solitary waves” (e.g., Song P et al, 1992, 1994; Baumgärtel, 1999; Lucek et al, 1999; Horbury et al, 2004; Stasiewicz, 2004; Tsurutani et al, 2011; Yao ST et al, 2018b; Tian AM et al, 2018, 2020; Zhang L et al, 2018; Treumann and Baumjohann, 2019; Wang GQ et al, 2020a; Kitamura et al, 2020). Of these terms, the first two describe the observable phenomenon, while the last two emphasize the generation mechanism and nature.…”