2023
DOI: 10.3847/1538-4357/acdc1c
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Kinetic Equilibrium of Two-dimensional Force-free Current Sheets

Abstract: Force-free current sheets are local plasma structures with field-aligned electric currents and approximately uniform plasma pressures. Such structures, widely found throughout the heliosphere, are sites for plasma instabilities and magnetic reconnection, the growth rate of which is controlled by the structure’s current-sheet configuration. Despite the fact that many kinetic equilibrium models have been developed for one-dimensional force-free current sheets, their two-dimensional (2D) counterparts, which have … Show more

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Cited by 3 publications
(3 citation statements)
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“…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. Moreover, observations of such partially force-free CSs provide a unique opportunity for the verification of models describing equilibrium for CSs without a normal magnetic field component, B n = 0, (e.g., Allanson et al, 2015;Neukirch, Vasko, et al, 2020, and references therein) and with a finite B n ≠ 0 (e.g., An et al, 2023;Artemyev, 2011;Mingalev et al, 2012;Vasko et al, 2014).…”
Section: Conclusion and Discussionmentioning
confidence: 99%
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“…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. Moreover, observations of such partially force-free CSs provide a unique opportunity for the verification of models describing equilibrium for CSs without a normal magnetic field component, B n = 0, (e.g., Allanson et al, 2015;Neukirch, Vasko, et al, 2020, and references therein) and with a finite B n ≠ 0 (e.g., An et al, 2023;Artemyev, 2011;Mingalev et al, 2012;Vasko et al, 2014).…”
Section: Conclusion and Discussionmentioning
confidence: 99%
“…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.…”
Section: Conclusion and Discussionmentioning
confidence: 99%
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