Induced Magnetic Fields and Plasma Motions in the Inner Part of the Martian Magnetosphere.
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| Title: | Induced Magnetic Fields and Plasma Motions in the Inner Part of the Martian Magnetosphere. |
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| Authors: | Dubinin, E.1 dubinin@mps.mpg.de, Fraenz, M.1, Modolo, R.2, Pätzold, M.3, Tellmann, S.3, Vaisberg, O.4, Shuvalov, S.4, Zelenyi, L.4, Chai, L.5, Wei, Y.5, McFadden, J.6, DiBraccio, G.7, Espley, J.7 |
| Source: | Journal of Geophysical Research. Space Physics. Dec2021, Vol. 126 Issue 12, p1-15. 15p. |
| Subject Terms: | Magnetic fields, Space plasmas, Magnetosphere, Martian atmosphere, Ionospheric plasma |
| Abstract: | Analysis of Mars Atmosphere and Volatile Evolution (MAVEN)/Supra‐Thermal And Thermal Ion Composition observations in the Martian upper atmosphere, bounded at higher altitudes by the shocked solar wind, shows that the draping of interplanetary magnetic field penetrates down to low altitudes (∼200−250 km) and governs dynamics of the ionosphere. The upper ionospheric plasma is driven into motion flowing around Mars similar to the shocked solar wind in the adjacent magnetosheath. Such a fluid‐like motion is accompanied by ion acceleration caused by the bending of the magnetic field, leading to ion extraction and finally to ion pickup. Extraction of ions and their acceleration produces a recoil effect of the bulk ionosphere in the opposite direction. This provides a strong asymmetry in ion dynamics in two different hemispheres, accompanied by wrapping of the magnetic field lines around Mars and respective reconnection. Plain Language Summary: Although the Martian magnetosphere is hybrid and contains components of the induced and intrinsic magnetosphere, is possible to display these components by using the specific coordinate systems. Here we study the properties of the induced magnetosphere using the data obtained by MAVEN spacecraft. The interplanetary magnetic field penetrates deep into the Martian ionosphere draping around Mars and drive to the motion dense ionospheric plasma. Draping features and the induced plasma motions occur different in two hemispheres determined by the direction of the motional electric field in the solar wind. Ion acceleration and extraction is accompanied by a recoil effect that leads to a shift and asymmetry of the ionosphere. Key Points: Draping of the interplanetary magnetic field around Mars penetrates deep to the ionosphere enveloping the planet and driving the ionosphere to the bulk motionDraping and motion of the ionospheric plasma is characterized by asymmetry by the direction of the motional electric field in solar windIon acceleration and extraction from the ionosphere is accompanied by a shift of the bulk ionosphere in the opposite direction [ABSTRACT FROM AUTHOR] |
| Copyright of Journal of Geophysical Research. Space Physics is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.) | |
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| Header | DbId: 8gh DbLabel: GreenFILE An: 154358598 AccessLevel: 6 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 0 |
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| Items | – Name: Title Label: Title Group: Ti Data: Induced Magnetic Fields and Plasma Motions in the Inner Part of the Martian Magnetosphere. – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22Dubinin%2C+E%2E%22">Dubinin, E.</searchLink><relatesTo>1</relatesTo><i> dubinin@mps.mpg.de</i><br /><searchLink fieldCode="AR" term="%22Fraenz%2C+M%2E%22">Fraenz, M.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Modolo%2C+R%2E%22">Modolo, R.</searchLink><relatesTo>2</relatesTo><br /><searchLink fieldCode="AR" term="%22Pätzold%2C+M%2E%22">Pätzold, M.</searchLink><relatesTo>3</relatesTo><br /><searchLink fieldCode="AR" term="%22Tellmann%2C+S%2E%22">Tellmann, S.</searchLink><relatesTo>3</relatesTo><br /><searchLink fieldCode="AR" term="%22Vaisberg%2C+O%2E%22">Vaisberg, O.</searchLink><relatesTo>4</relatesTo><br /><searchLink fieldCode="AR" term="%22Shuvalov%2C+S%2E%22">Shuvalov, S.</searchLink><relatesTo>4</relatesTo><br /><searchLink fieldCode="AR" term="%22Zelenyi%2C+L%2E%22">Zelenyi, L.</searchLink><relatesTo>4</relatesTo><br /><searchLink fieldCode="AR" term="%22Chai%2C+L%2E%22">Chai, L.</searchLink><relatesTo>5</relatesTo><br /><searchLink fieldCode="AR" term="%22Wei%2C+Y%2E%22">Wei, Y.</searchLink><relatesTo>5</relatesTo><br /><searchLink fieldCode="AR" term="%22McFadden%2C+J%2E%22">McFadden, J.</searchLink><relatesTo>6</relatesTo><br /><searchLink fieldCode="AR" term="%22DiBraccio%2C+G%2E%22">DiBraccio, G.</searchLink><relatesTo>7</relatesTo><br /><searchLink fieldCode="AR" term="%22Espley%2C+J%2E%22">Espley, J.</searchLink><relatesTo>7</relatesTo> – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Journal+of+Geophysical+Research%2E+Space+Physics%22">Journal of Geophysical Research. Space Physics</searchLink>. Dec2021, Vol. 126 Issue 12, p1-15. 15p. – Name: Subject Label: Subject Terms Group: Su Data: <searchLink fieldCode="DE" term="%22Magnetic+fields%22">Magnetic fields</searchLink><br /><searchLink fieldCode="DE" term="%22Space+plasmas%22">Space plasmas</searchLink><br /><searchLink fieldCode="DE" term="%22Magnetosphere%22">Magnetosphere</searchLink><br /><searchLink fieldCode="DE" term="%22Martian+atmosphere%22">Martian atmosphere</searchLink><br /><searchLink fieldCode="DE" term="%22Ionospheric+plasma%22">Ionospheric plasma</searchLink> – Name: Abstract Label: Abstract Group: Ab Data: Analysis of Mars Atmosphere and Volatile Evolution (MAVEN)/Supra‐Thermal And Thermal Ion Composition observations in the Martian upper atmosphere, bounded at higher altitudes by the shocked solar wind, shows that the draping of interplanetary magnetic field penetrates down to low altitudes (∼200−250 km) and governs dynamics of the ionosphere. The upper ionospheric plasma is driven into motion flowing around Mars similar to the shocked solar wind in the adjacent magnetosheath. Such a fluid‐like motion is accompanied by ion acceleration caused by the bending of the magnetic field, leading to ion extraction and finally to ion pickup. Extraction of ions and their acceleration produces a recoil effect of the bulk ionosphere in the opposite direction. This provides a strong asymmetry in ion dynamics in two different hemispheres, accompanied by wrapping of the magnetic field lines around Mars and respective reconnection. Plain Language Summary: Although the Martian magnetosphere is hybrid and contains components of the induced and intrinsic magnetosphere, is possible to display these components by using the specific coordinate systems. Here we study the properties of the induced magnetosphere using the data obtained by MAVEN spacecraft. The interplanetary magnetic field penetrates deep into the Martian ionosphere draping around Mars and drive to the motion dense ionospheric plasma. Draping features and the induced plasma motions occur different in two hemispheres determined by the direction of the motional electric field in the solar wind. Ion acceleration and extraction is accompanied by a recoil effect that leads to a shift and asymmetry of the ionosphere. Key Points: Draping of the interplanetary magnetic field around Mars penetrates deep to the ionosphere enveloping the planet and driving the ionosphere to the bulk motionDraping and motion of the ionospheric plasma is characterized by asymmetry by the direction of the motional electric field in solar windIon acceleration and extraction from the ionosphere is accompanied by a shift of the bulk ionosphere in the opposite direction [ABSTRACT FROM AUTHOR] – Name: AbstractSuppliedCopyright Label: Group: Ab Data: <i>Copyright of Journal of Geophysical Research. Space Physics is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.) |
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| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1029/2021JA029542 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 15 StartPage: 1 Subjects: – SubjectFull: Magnetic fields Type: general – SubjectFull: Space plasmas Type: general – SubjectFull: Magnetosphere Type: general – SubjectFull: Martian atmosphere Type: general – SubjectFull: Ionospheric plasma Type: general Titles: – TitleFull: Induced Magnetic Fields and Plasma Motions in the Inner Part of the Martian Magnetosphere. Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Dubinin, E. – PersonEntity: Name: NameFull: Fraenz, M. – PersonEntity: Name: NameFull: Modolo, R. – PersonEntity: Name: NameFull: Pätzold, M. – PersonEntity: Name: NameFull: Tellmann, S. – PersonEntity: Name: NameFull: Vaisberg, O. – PersonEntity: Name: NameFull: Shuvalov, S. – PersonEntity: Name: NameFull: Zelenyi, L. – PersonEntity: Name: NameFull: Chai, L. – PersonEntity: Name: NameFull: Wei, Y. – PersonEntity: Name: NameFull: McFadden, J. – PersonEntity: Name: NameFull: DiBraccio, G. – PersonEntity: Name: NameFull: Espley, J. IsPartOfRelationships: – BibEntity: Dates: – D: 01 M: 12 Text: Dec2021 Type: published Y: 2021 Identifiers: – Type: issn-print Value: 21699380 Numbering: – Type: volume Value: 126 – Type: issue Value: 12 Titles: – TitleFull: Journal of Geophysical Research. Space Physics Type: main |
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