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Ion‐Mediated Tearing and Kink Instabilities in the Earth's Magnetosphere: Hybrid‐Vlasov Simulations.

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Title: Ion‐Mediated Tearing and Kink Instabilities in the Earth's Magnetosphere: Hybrid‐Vlasov Simulations.
Authors: Zaitsev, I.1 (AUTHOR) ivan.zaitsev@helsinki.fi, Cozzani, G.1 (AUTHOR), Alho, M.1 (AUTHOR), Horaites, K.1 (AUTHOR), Zhou, H.2 (AUTHOR), Kit, A.3 (AUTHOR), Pfau‐Kempf, Y.1 (AUTHOR), Hoilijoki, S.1 (AUTHOR), Ganse, U.1 (AUTHOR), Battarbee, M.1 (AUTHOR), Papadakis, K.1 (AUTHOR), Suni, J.1 (AUTHOR), Dubart, M.4 (AUTHOR), Tesema‐Kebede, F.5 (AUTHOR), Workayehu, A.1 (AUTHOR), Tarvus, V.1 (AUTHOR), Kotipalo, L.1 (AUTHOR), Koikkalainen, V.1 (AUTHOR), Turc, L.1 (AUTHOR), Palmroth, M.1,6 (AUTHOR)
Source: Journal of Geophysical Research. Space Physics. Jan2025, Vol. 130 Issue 1, p1-16. 16p.
Subject Terms: Current sheets, Ion sources, Magnetosphere, Warehouses, Current distribution
Abstract: We explore the three‐dimensional structure of ion‐kinetic instabilities in a thin current layer using a hybrid‐Vlasov simulation of the Earth's magnetosphere. The simulation shows the simultaneous growth of tearing and kinking instabilities, which develop in the Sun‐Earth and dawn‐dusk directions, respectively, within the magnetotail current sheet. The formation of flux ropes indicates the development of the tearing instability, while flapping‐type cross‐tail oscillations arise from the kink instability. We consider both instabilities as independent polarizations, albeit sharing a common source: demagnetized ions forming crescent‐shape distributions at the center of the current layer. These oscillations exhibit spatiotemporal characteristics within the proton‐scale range, featuring a growth time on the order of 40–80 proton gyroperiods and a wavelength of approximately 15–30 proton skin depths. Key Points: The growth rate of magnetic islands corresponds to the prediction of ion tearing instability in the Earth's magnetotailAcceleration of protons along X‐lines forming due to the tearing instability amplifies the current sheet kinking on the duskward sideKink instability causes ion scale flapping [ABSTRACT FROM AUTHOR]
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Abstract:We explore the three‐dimensional structure of ion‐kinetic instabilities in a thin current layer using a hybrid‐Vlasov simulation of the Earth's magnetosphere. The simulation shows the simultaneous growth of tearing and kinking instabilities, which develop in the Sun‐Earth and dawn‐dusk directions, respectively, within the magnetotail current sheet. The formation of flux ropes indicates the development of the tearing instability, while flapping‐type cross‐tail oscillations arise from the kink instability. We consider both instabilities as independent polarizations, albeit sharing a common source: demagnetized ions forming crescent‐shape distributions at the center of the current layer. These oscillations exhibit spatiotemporal characteristics within the proton‐scale range, featuring a growth time on the order of 40–80 proton gyroperiods and a wavelength of approximately 15–30 proton skin depths. Key Points: The growth rate of magnetic islands corresponds to the prediction of ion tearing instability in the Earth's magnetotailAcceleration of protons along X‐lines forming due to the tearing instability amplifies the current sheet kinking on the duskward sideKink instability causes ion scale flapping [ABSTRACT FROM AUTHOR]
ISSN:21699380
DOI:10.1029/2024JA032615