2019
DOI: 10.3847/2041-8213/ab21c8
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Properties of the Turbulence Associated with Electron-only Magnetic Reconnection in Earth’s Magnetosheath

Abstract: 21 Corresponding author: J. E. Stawarz j.stawarz@imperial.ac.uk 2 Turbulent plasmas generate intense current structures, which have long been sug-22 gested as magnetic reconnection sites. Recent Magnetospheric Multiscale (MMS) ob-23 servations in Earth's magnetosheath revealed a novel form of reconnection where the 24 dynamics only couple to electrons, without ion involvement. It was suggested that 25 such dynamics were driven by magnetosheath turbulence. In this study, the fluctua-26 tions are examined to det… Show more

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Cited by 94 publications
(122 citation statements)
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“…The essential physical result is that if the initial collapsing solution is not sufficiently anisotropic when its thickness is above the ion scales, the collapse continues down to a thickness well below the ion scale, and electron-only reconnection will occur. Remarkably (considering the formal limitation of KREHM to low β), we will see that our model seems to agree rather well with the magnetosheath observations of electron-only reconnection (Phan et al 2018;Stawarz et al 2019).…”
Section: Introductionsupporting
confidence: 82%
“…The essential physical result is that if the initial collapsing solution is not sufficiently anisotropic when its thickness is above the ion scales, the collapse continues down to a thickness well below the ion scale, and electron-only reconnection will occur. Remarkably (considering the formal limitation of KREHM to low β), we will see that our model seems to agree rather well with the magnetosheath observations of electron-only reconnection (Phan et al 2018;Stawarz et al 2019).…”
Section: Introductionsupporting
confidence: 82%
“…Analysis of the location of active reconnection sites associated with shock waves has shown that the phenomenon is localized to the shock and thus separated from turbulent reconnection occurring in the magnetosheath (Phan et al, ; Stawarz et al, ). This is consistent with the expectations set by hybrid simulations of Earth's bow shock presented by Gingell et al (), which show that reconnection sites are generated on sub‐ion timescales in a transient, localized transition region.…”
Section: Discussionmentioning
confidence: 99%
“…It is interesting to analyze this result in light of recent MMS observations of so-called electron-only reconnection in the Earth's magnetosheath (Phan et al 2018;Stawarz et al 2019). In Boldyrev & Loureiro (2019) we have estimated that the decoupling of the ions in these events requires λ/d e ≪ d i /d e or λ/d e ≪ (d i /d e ) 2/3 depending on whether one assumes a tanh(x/λ) or sin(x/λ) magnetic field profile for the reconnecting field B ξ (x) in the eddy.…”
Section: Reconnection At Kinetic Scalesmentioning
confidence: 99%