Hybrid simulation of comet Shoemaker-Levy 9 interaction with Jovian bow shock

dc.contributor.authorLipatov, Alexander
dc.contributor.authorSharma, A. S.
dc.date.accessioned2024-01-30T07:46:46Z
dc.date.available2024-01-30T07:46:46Z
dc.date.issued1994-06-01
dc.description.abstractThe interaction of the solar wind with comet Shoemaker-Levy 9 leading to the formation of the cometary magnetosphere and its interaction with the Jovian bow shock is simulated using a one dimensional hybrid code. The mass loading of the solar wind by the cometary ions leads to the formation of a bow shock behind which the plasma density is 2–3 cm⁻³ and the electron temperature is 4 eV. The interaction of this system with the Jovian bow shock yields local enhancements of the magnetic field and the plasma density by factors of 4-5 and the electron temperature by 2-3.
dc.description.sponsorshipThis work was supported by NASA and NSF grants. We acknowledge many fruitful discussions with G. M. Milikh, K. Papadopoulos and R. Z. Sagdeer. The computations were performed at the UMD Advanced Visualization Laboratory.
dc.description.urihttps://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/94GL01295
dc.format.extent4 pages
dc.genrejournal articles
dc.identifier.citationLipatov, A. S., and A. S. Sharma. “Hybrid Simulation of Comet Shoemaker-Levy 9 Interaction with Jovian Bow Shock.” Geophysical Research Letters 21, no. 11 (1994): 1059–62. https://doi.org/10.1029/94GL01295.
dc.identifier.urihttps://doi.org/10.1029/94GL01295
dc.identifier.urihttp://hdl.handle.net/11603/31518
dc.language.isoen_US
dc.publisherAGU
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Goddard Planetary Heliophysics Institute (GPHI)
dc.relation.ispartofUMBC GESTAR II
dc.rights©1994. American Geophysical Union. All Rights Reserved
dc.titleHybrid simulation of comet Shoemaker-Levy 9 interaction with Jovian bow shock
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0001-5026-8214

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