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Magnetospheric Sources of Theta Aurora: A Case Study Comparing Observations With SWMF Global Simulation
Department of Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI, USA.
Department of Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI, USA.
Department of Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI, USA.
Department of Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI, USA; West Virginia University, Morgantown, WV, USA.
Vise andre og tillknytning
2024 (engelsk)Inngår i: Geophysical Research Letters, ISSN 0094-8276, E-ISSN 1944-8007, Vol. 51, nr 10, artikkel-id e2023GL108002Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

We present the first high resolution global MHD with coupled inner magnetosphere simulation results of an observed theta aurora event. We use the Space Weather Modeling Framework in the Geospace configuration, which produces accurate field aligned current closure in the ionosphere that is integral to theta aurora formation. At the location of the observed theta aurora, the simulation produces a narrow channel of Joule heating along both open and closed field lines, and between a pair of oppositely directed field-aligned current sheets in the ionosphere. We demonstrate that this Joule heating pattern that we identify as theta aurora maps to a reconnection region at the magnetotail flanks as well as in the distant magnetotail. The theta aurora maps to a cross-tail current disruption and field-aligned current source region in a highly twisted magnetotail.

sted, utgiver, år, opplag, sider
American Geophysical Union (AGU) , 2024. Vol. 51, nr 10, artikkel-id e2023GL108002
Emneord [en]
ionosphere, magnetotail, reconnection, simulation, theta aurora, transpolar arc
HSV kategori
Identifikatorer
URN: urn:nbn:se:kth:diva-347050DOI: 10.1029/2023GL108002ISI: 001228247000001Scopus ID: 2-s2.0-85193781821OAI: oai:DiVA.org:kth-347050DiVA, id: diva2:1862778
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QC 20240531

Tilgjengelig fra: 2024-05-30 Laget: 2024-05-30 Sist oppdatert: 2024-06-04bibliografisk kontrollert

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