2016
DOI: 10.3847/0004-637x/822/1/38
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Multiple Current Sheet Systems in the Outer Heliosphere: Energy Release and Turbulence

Abstract: In the outer heliosphere, beyond the solar wind termination shock, it is expected that the warped heliospheric current sheet forms a region of closelypacked, multiple, thin current sheets. Such a system may be subject to the ion-kinetic tearing instability, and hence generate magnetic islands and hot populations of ions associated with magnetic reconnection. Reconnection processes in this environment have important implications for local particle transport, and for particle acceleration at reconnection sites a… Show more

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Cited by 19 publications
(27 citation statements)
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“…The multiple current sheet system is itself anisotropic, however in the AP case fast growth of the tearing instability and associated fluctuations evolve the system towards an approximately isotropic state by tΩ i 25. However, the guide field is known to introduce anisotropy in the magnetic spectrum of an MCS system (Burgess et al 2016). In the GF case, a relative reduction in the power in the parallel direction compared to the perpendicular direction, visible also in the magnetic structure in figure 1(b), leads to an effective reduction of the spectral index for the isotropically integrated spectrum.…”
Section: Resultsmentioning
confidence: 99%
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“…The multiple current sheet system is itself anisotropic, however in the AP case fast growth of the tearing instability and associated fluctuations evolve the system towards an approximately isotropic state by tΩ i 25. However, the guide field is known to introduce anisotropy in the magnetic spectrum of an MCS system (Burgess et al 2016). In the GF case, a relative reduction in the power in the parallel direction compared to the perpendicular direction, visible also in the magnetic structure in figure 1(b), leads to an effective reduction of the spectral index for the isotropically integrated spectrum.…”
Section: Resultsmentioning
confidence: 99%
“…the development of magnetic islands of varying scales, without the clutter of following multiple field lines in three dimensions. The time evolution of the tearing instability and associated magnetic structure for these multiple current sheet systems is described in detail by Burgess et al (2016). Discussion of the effects of other instabilities on the evolution of single three-dimensional ion-scale current sheets, including the drift-kink, firehose and ion cyclotron instabilities, can be found in Gingell et al (2015).…”
Section: Resultsmentioning
confidence: 99%
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