Reconnection X‐Line Orientations at the Earth's Magnetopause.

Saved in:
Bibliographic Details
Title: Reconnection X‐Line Orientations at the Earth's Magnetopause.
Authors: Fuselier, S. A.1,2 sfuselier@swri.edu, Webster, J. M.1,3, Trattner, K. J.4, Petrinec, S. M.5, Genestreti, K. J.6, Pritchard, K. R.1,2, LLera, K.1, Broll, J. M.7, Burch, J. L.1, Strangeway, R. J.8
Source: Journal of Geophysical Research. Space Physics. Dec2021, Vol. 126 Issue 12, p1-16. 16p.
Subject Terms: Magnetopause, Electron diffusion, Atmospheric magnetism, Interplanetary magnetic fields, Laser atmospheric observations, Magnetic reconnection
Abstract: Observations from the magnetospheric multiscale mission in or near electron diffusion regions (EDRs) at the Earth's magnetopause are used to determine the orientation of reconnection X‐lines. The results highlight cross‐scale coupling of magnetic reconnection and the differences between component and anti‐parallel reconnection. These observations are consistent with a model that has a continuous, component reconnection X‐line that extends many Earth Radii (RE) across the dayside magnetopause when the interplanetary magnetic field (IMF) is southward and |BY| ∼ |BZ|. Encounters anywhere along the X‐line have similar cross‐section structure in the direction normal to the magnetopause, indicating that component reconnection is quasi‐two‐dimensional, at some scale larger than the electron scale. EDR encounters far from this primary component X‐line may be associated with transient or spatially limited reconnection structures. On the magnetopause flanks on either side of the component X‐line, there are regions where anti‐parallel reconnection occurs. These regions dominate the entire dayside magnetopause when the IMF is southward and |BY| << |BZ|. In parts of these regions, observations in or near EDRs are consistent with reconnection occurring at a series of short, anti‐parallel reconnection X‐lines. These X‐lines may be quasi‐stationary or propagating along an anti‐parallel ridge at the magnetopause. In other parts of these regions, X‐lines may be much longer. Plain Language Summary: Magnetic reconnection is the process that couples the solar wind and the Earth's magnetosphere. This process produces long reconnection lines that stretch across the Earth's magnetopause. This paper describes the orientation of these reconnection lines. Key Points: Magnetospheric multiscale observations are used to determine the orientation of reconnection X‐lines at the Earth's magnetopauseFor southward interplanetary magnetic field and BY ∼ BZ, there is a long, continuous, component reconnection X‐line extending many RE across the dayside magnetopauseIn high shear regions, there may be many, short, anti‐parallel reconnection X‐lines or a long X‐line along a high magnetic shear ridge [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.)
Database: GreenFILE
FullText Text:
  Availability: 0
Header DbId: 8gh
DbLabel: GreenFILE
An: 154358564
AccessLevel: 6
PubType: Academic Journal
PubTypeId: academicJournal
PreciseRelevancyScore: 0
IllustrationInfo
Items – Name: Title
  Label: Title
  Group: Ti
  Data: Reconnection X‐Line Orientations at the Earth&#39;s Magnetopause.
– Name: Author
  Label: Authors
  Group: Au
  Data: &lt;searchLink fieldCode=&quot;AR&quot; term=&quot;%22Fuselier%2C+S%2E+A%2E%22&quot;&gt;Fuselier, S. A.&lt;/searchLink&gt;&lt;relatesTo&gt;1,2&lt;/relatesTo&gt;&lt;i&gt; sfuselier@swri.edu&lt;/i&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;AR&quot; term=&quot;%22Webster%2C+J%2E+M%2E%22&quot;&gt;Webster, J. M.&lt;/searchLink&gt;&lt;relatesTo&gt;1,3&lt;/relatesTo&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;AR&quot; term=&quot;%22Trattner%2C+K%2E+J%2E%22&quot;&gt;Trattner, K. J.&lt;/searchLink&gt;&lt;relatesTo&gt;4&lt;/relatesTo&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;AR&quot; term=&quot;%22Petrinec%2C+S%2E+M%2E%22&quot;&gt;Petrinec, S. M.&lt;/searchLink&gt;&lt;relatesTo&gt;5&lt;/relatesTo&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;AR&quot; term=&quot;%22Genestreti%2C+K%2E+J%2E%22&quot;&gt;Genestreti, K. J.&lt;/searchLink&gt;&lt;relatesTo&gt;6&lt;/relatesTo&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;AR&quot; term=&quot;%22Pritchard%2C+K%2E+R%2E%22&quot;&gt;Pritchard, K. R.&lt;/searchLink&gt;&lt;relatesTo&gt;1,2&lt;/relatesTo&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;AR&quot; term=&quot;%22LLera%2C+K%2E%22&quot;&gt;LLera, K.&lt;/searchLink&gt;&lt;relatesTo&gt;1&lt;/relatesTo&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;AR&quot; term=&quot;%22Broll%2C+J%2E+M%2E%22&quot;&gt;Broll, J. M.&lt;/searchLink&gt;&lt;relatesTo&gt;7&lt;/relatesTo&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;AR&quot; term=&quot;%22Burch%2C+J%2E+L%2E%22&quot;&gt;Burch, J. L.&lt;/searchLink&gt;&lt;relatesTo&gt;1&lt;/relatesTo&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;AR&quot; term=&quot;%22Strangeway%2C+R%2E+J%2E%22&quot;&gt;Strangeway, R. J.&lt;/searchLink&gt;&lt;relatesTo&gt;8&lt;/relatesTo&gt;
– Name: TitleSource
  Label: Source
  Group: Src
  Data: &lt;searchLink fieldCode=&quot;JN&quot; term=&quot;%22Journal+of+Geophysical+Research%2E+Space+Physics%22&quot;&gt;Journal of Geophysical Research. Space Physics&lt;/searchLink&gt;. Dec2021, Vol. 126 Issue 12, p1-16. 16p.
– Name: Subject
  Label: Subject Terms
  Group: Su
  Data: &lt;searchLink fieldCode=&quot;DE&quot; term=&quot;%22Magnetopause%22&quot;&gt;Magnetopause&lt;/searchLink&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;DE&quot; term=&quot;%22Electron+diffusion%22&quot;&gt;Electron diffusion&lt;/searchLink&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;DE&quot; term=&quot;%22Atmospheric+magnetism%22&quot;&gt;Atmospheric magnetism&lt;/searchLink&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;DE&quot; term=&quot;%22Interplanetary+magnetic+fields%22&quot;&gt;Interplanetary magnetic fields&lt;/searchLink&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;DE&quot; term=&quot;%22Laser+atmospheric+observations%22&quot;&gt;Laser atmospheric observations&lt;/searchLink&gt;&lt;br /&gt;&lt;searchLink fieldCode=&quot;DE&quot; term=&quot;%22Magnetic+reconnection%22&quot;&gt;Magnetic reconnection&lt;/searchLink&gt;
– Name: Abstract
  Label: Abstract
  Group: Ab
  Data: Observations from the magnetospheric multiscale mission in or near electron diffusion regions (EDRs) at the Earth&#39;s magnetopause are used to determine the orientation of reconnection X‐lines. The results highlight cross‐scale coupling of magnetic reconnection and the differences between component and anti‐parallel reconnection. These observations are consistent with a model that has a continuous, component reconnection X‐line that extends many Earth Radii (RE) across the dayside magnetopause when the interplanetary magnetic field (IMF) is southward and |BY| ∼ |BZ|. Encounters anywhere along the X‐line have similar cross‐section structure in the direction normal to the magnetopause, indicating that component reconnection is quasi‐two‐dimensional, at some scale larger than the electron scale. EDR encounters far from this primary component X‐line may be associated with transient or spatially limited reconnection structures. On the magnetopause flanks on either side of the component X‐line, there are regions where anti‐parallel reconnection occurs. These regions dominate the entire dayside magnetopause when the IMF is southward and |BY| &lt;&lt; |BZ|. In parts of these regions, observations in or near EDRs are consistent with reconnection occurring at a series of short, anti‐parallel reconnection X‐lines. These X‐lines may be quasi‐stationary or propagating along an anti‐parallel ridge at the magnetopause. In other parts of these regions, X‐lines may be much longer. Plain Language Summary: Magnetic reconnection is the process that couples the solar wind and the Earth&#39;s magnetosphere. This process produces long reconnection lines that stretch across the Earth&#39;s magnetopause. This paper describes the orientation of these reconnection lines. Key Points: Magnetospheric multiscale observations are used to determine the orientation of reconnection X‐lines at the Earth&#39;s magnetopauseFor southward interplanetary magnetic field and BY ∼ BZ, there is a long, continuous, component reconnection X‐line extending many RE across the dayside magnetopauseIn high shear regions, there may be many, short, anti‐parallel reconnection X‐lines or a long X‐line along a high magnetic shear ridge [ABSTRACT FROM AUTHOR]
– Name: AbstractSuppliedCopyright
  Label:
  Group: Ab
  Data: &lt;i&gt;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&#39;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.&lt;/i&gt; (Copyright applies to all Abstracts.)
PLink https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&db=8gh&AN=154358564
RecordInfo BibRecord:
  BibEntity:
    Identifiers:
      – Type: doi
        Value: 10.1029/2021JA029789
    Languages:
      – Code: eng
        Text: English
    PhysicalDescription:
      Pagination:
        PageCount: 16
        StartPage: 1
    Subjects:
      – SubjectFull: Magnetopause
        Type: general
      – SubjectFull: Electron diffusion
        Type: general
      – SubjectFull: Atmospheric magnetism
        Type: general
      – SubjectFull: Interplanetary magnetic fields
        Type: general
      – SubjectFull: Laser atmospheric observations
        Type: general
      – SubjectFull: Magnetic reconnection
        Type: general
    Titles:
      – TitleFull: Reconnection X‐Line Orientations at the Earth's Magnetopause.
        Type: main
  BibRelationships:
    HasContributorRelationships:
      – PersonEntity:
          Name:
            NameFull: Fuselier, S. A.
      – PersonEntity:
          Name:
            NameFull: Webster, J. M.
      – PersonEntity:
          Name:
            NameFull: Trattner, K. J.
      – PersonEntity:
          Name:
            NameFull: Petrinec, S. M.
      – PersonEntity:
          Name:
            NameFull: Genestreti, K. J.
      – PersonEntity:
          Name:
            NameFull: Pritchard, K. R.
      – PersonEntity:
          Name:
            NameFull: LLera, K.
      – PersonEntity:
          Name:
            NameFull: Broll, J. M.
      – PersonEntity:
          Name:
            NameFull: Burch, J. L.
      – PersonEntity:
          Name:
            NameFull: Strangeway, R. 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
ResultId 1