Overlapping cusp ion dispersions formed by flux ropes on the day-side magnetopause

dc.contributor.authorPetrinec, Steven
dc.contributor.authorConnor, Hyunju K.
dc.contributor.authorda Silva, Daniel
dc.contributor.authorMa, Xuanye
dc.contributor.authorDorelli, John C.
dc.contributor.authorPorter, Azzan
dc.contributor.authorGirma, Yohannes
dc.contributor.authorBurkholder, Brandon
dc.date.accessioned2024-11-14T15:18:53Z
dc.date.available2024-11-14T15:18:53Z
dc.date.issued2024-08-20
dc.description.abstractIntroduction: Cusp ion dispersion signatures reflect properties of remote magnetic reconnection. Since the cusp is easier to observe in situ compared to the reconnection x-line, ion dispersions provide key insight on whether reconnection is variable in space and time. This study is motivated by a specific dispersion signature having two ion populations separated in energy but not space. These are known as overlapping dispersions because when observed by low-Earth orbiting satellites traversing the cusp, they appear as two dispersed ion populations overlapping in magnetic latitudes. Overlapping dispersion signatures have been observed for all interplanetary magnetic field (IMF) orientations and have been associated with multiple reconnection processes, but the three-dimensional magnetic reconnection topology and particle trajectories have not been examined.Methods: Forward particle tracing using the GAMERA-CHIMP global magnetohydrodynamic (MHD) with test particle framework is carried out to construct ion dispersion signatures throughout the cusp. Under idealized solar wind driving with steady purely southward IMF, both standard and overlapping dispersions are found.Results: Analysis of the test particle trajectories shows that the higher energy population of the overlapping dispersion travels along the axis of a flux rope before heading into the cusp, whereas the lower energy population goes directly into the cusp. Furthermore, the overlapping dispersions observed by the synthetic satellites compare well to Defense Meteorological Satellite Program (DMSP) F16 observations during strongly southward IMF.Discussion: It is thus concluded that during strongly southward IMF, cusp-entering particles interacting with a magnetopause flux rope (generated by secondary reconnection) is one way to produce an overlapping dispersion. This study lays the groundwork for the forthcoming NASA Tandem Reconnection and Cusp Electrodynamics Reconnaissance Satellites (TRACERS) mission, which will connect the cusp to the magnetosphere—discovering how spatial or temporal variations in magnetic reconnection drive cusp dynamics. The expected launch of TRACERS is in 2025.
dc.description.sponsorshipThe author(s) declare that financial support was received for the research, authorship, and/or publication of this article. This work is provided by NASA Magnetospheric Multiscale (MMS) Early Career Grant 80NSSC22K0949.
dc.description.urihttps://www.frontiersin.org/journals/astronomy-and-space-sciences/articles/10.3389/fspas.2024.1430966/full
dc.format.extent14 pages
dc.genrejournal articles
dc.identifierdoi:10.13016/m2grsi-yqbw
dc.identifier.citationPetrinec, Steven, Hyunju K. Connor, Daniel da Silva, Xuanye Ma, John C. Dorelli, Azzan Porter, Yohannes Girma, and Brandon Burkholder. “Overlapping Cusp Ion Dispersions Formed by Flux Ropes on the Day-Side Magnetopause.” Frontiers in Astronomy and Space Sciences 11 (August 21, 2024). https://doi.org/10.3389/fspas.2024.1430966.
dc.identifier.urihttps://doi.org/10.3389/fspas.2024.1430966
dc.identifier.urihttp://hdl.handle.net/11603/36971
dc.language.isoen_US
dc.publisherfrontiers
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Goddard Planetary Heliophysics Institute (GPHI)
dc.relation.ispartofUMBC Faculty Collection
dc.relation.ispartofUMBC Physics Department
dc.relation.ispartofUMBC Mathematics and Statistics Department
dc.relation.ispartofUMBC Student Collection
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.rightsPublic Domain
dc.rights.urihttps://creativecommons.org/publicdomain/mark/1.0/
dc.subjectmagnetic reconnection
dc.subjectcusp dispersion
dc.subjectflux transfer events
dc.subjectglobal simulation
dc.subjection dynamics
dc.subjectmagnetic flux ropes
dc.subjectmagnetohydrodynamics
dc.subjecttest particles
dc.titleOverlapping cusp ion dispersions formed by flux ropes on the day-side magnetopause
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0001-7537-3539
dcterms.creatorhttps://orcid.org/0000-0001-8702-5806

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