Magnetopause Reconnection and Indents Induced by Foreshock Turbulence

dc.contributor.authorChen, Li-Jen
dc.contributor.authorNg, Jonathan
dc.contributor.authorOmelchenko, Yuri
dc.contributor.authorWang, Shan
dc.date.accessioned2021-07-28T14:48:57Z
dc.date.available2021-07-28T14:48:57Z
dc.date.issued2021-05-31
dc.description.abstractAbstract Based on global hybrid simulation results, we predict that foreshock turbulence can reach the magnetopause and lead to reconnection as well as Earth-sized indents. Both the interplanetary magnetic field (IMF) and solar wind are constant in our simulation, and hence, all dynamics are generated by foreshock instabilities. The IMF in the simulation is mostly Sun-Earth aligned with a weak northward and zero dawn-dusk component, such that subsolar magnetopause reconnection is not expected without foreshock turbulence modifying the magnetosheath fields. We show a reconnection example to illustrate that the turbulence can create large magnetic shear angles across the magnetopause to induce local bursty reconnection. Magnetopause reconnection and indents developed from the impact of foreshock turbulence can potentially contribute to dayside loss of planetary plasmas. Plain Language Summary Turbulence structures are commonly generated as ions reflected by planetary bow shocks interact with the incoming solar wind. We use a large-scale simulation treating ions as particles and electrons as a fluid to investigate the impact of these turbulence structures on the magnetopsheres. Based on the simulation results, we predict that the turbulence can open magnetic field lines on the dayside and lead to planet-sized indents. Our work unfolds a potential pathway through which planetary plasmas can escape to the upstream solar wind.en_US
dc.description.sponsorshipThe research was supported in part by the MMS mission, DOE grants DESC0016278, DESC0020058, NSF AGS-1619584, AGS-2010231, and NASA 80NSSC18K1369 and 80NSSC19K0838. The authors thank Johnny Zhang, Michael Heinsohn, Nancy Carney, and other NASA Advanced-Supercomputing and High-End-Computing team members for their professional support to make the simulation possible.​ The simulation ran on 640 Pleiades Ivy Bridge nodes for 22 hours.en_US
dc.description.urihttps://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2021GL093029en_US
dc.format.extent7 pagesen_US
dc.genrejournal articlesen_US
dc.identifierdoi:10.13016/m27ynn-nm5r
dc.identifier.citationChen, Li-Jen et al.; Magnetopause Reconnection and Indents Induced by Foreshock Turbulence; Geophysical Research Letters, 48, 11, 31 May, 2021; https://doi.org/10.1029/2021GL093029en_US
dc.identifier.urihttps://doi.org/10.1029/2021GL093029
dc.identifier.urihttp://hdl.handle.net/11603/22194
dc.language.isoen_USen_US
dc.publisherAmerican Geophysical Unionen_US
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Goddard Planetary Heliophysics Institute (GPHI)
dc.rightsThis item is likely protected under Title 17 of the U.S. Copyright Law. Unless on a Creative Commons license, for uses protected by Copyright Law, contact the copyright holder or the author.
dc.rightsPublic Domain Mark 1.0*
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
dc.rights.urihttp://creativecommons.org/publicdomain/mark/1.0/*
dc.titleMagnetopause Reconnection and Indents Induced by Foreshock Turbulenceen_US
dc.typeTexten_US

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