“…Partially force-free CSs, which appear to make up a significant fraction of the middle magnetotail CSs, are rarely observed in the near-Earth magnetotail, where these CSs are usually associated with magnetic reconnection Nakamura et al, 2008). However, partially force-free CSs are much more typical in the solar wind (Artemyev, Angelopoulos, & Vasko, 2019;Lotekar et al, 2022;Neukirch, Vasko, et al, 2020), Earth magnetopause (e.g., Lukin et al, 2020;Panov et al, 2011), and planetary magnetospheres (e.g., Artemyev et al, 2014;DiBraccio et al, 2015;Rong et al, 2015), where their formation is associated with insufficient ion contribution to the pressure balance (see discussion in An et al, 2023). Therefore, our results confirm the idea of Liuzzo et al (2022), that the middle magnetotail is a natural plasma laboratory for in situ CS investigations across a wide range of plasma characteristics.…”