Full-particle simulations of instabilities in a thin current sheet of the magnetospheric system prior to substorm onset
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DOI[10.1186/s40623-015-0335-7]to the data of the same series
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- Material Type
- 記事
- Author/Editor
- Hirotoshi UchinoShinobu Machida
- Publication, Distribution, etc.
- Publication Date
- 2015-10-08
- Publication Date (W3CDTF)
- 2015-10-08
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 67(165)
- Volume
- 67(165)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-015-0335-7
- Persistent ID (NDL)
- info:ndljp/pid/9534538
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2015-11-16T20:25:38+09:00
- Date Captured (W3CDTF)
- 2015-10-20
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/9227920
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Summary, etc.
- Substorm triggering was the focus of recent two-dimensional superposed-epoch analyses based on Geotail and THEMIS data. The results indicate that magnetic-field dipolarization at X∼-8 Re and magnetic reconnection at X∼-20 Re occur simultaneously at the onset. These results imply that there are physical mechanisms that widely affect both the dipole and current-sheet regions. The analyses also have found that a local B z enhancement appears before the substorm onset and magnetic reconnection occurs at its tailward edge. We performed four 2.5-dimensional full-particle simulations with a new initial magnetic-field structure to focus on instabilities in the magnetosphere. The structure is similar to the Earth's dipole magnetic field combined with a stretched field and current sheet on the tailward side. The simulation with the initial magnetic-field configuration shows that nodes of the magnetic field appear in the current sheet where the growth condition of tearing instability is satisfied. The features of the instability are close to those of the electron tearing mode reported in previous simulation results. Another three simulations with a local B z enhancement, as seen in the observational results, at various locations in the current sheet were performed to explore its impacts on the evolution of the instability. A relaxation process around the enhancement generates a new node at its tailward edge if its location satisfies the growth condition. The wavelength and dominant mode of the instability can be changed by the coupling between the process and tearing mode depending on the location of the enhancement. Our simulations reveal new features associated with tearing instabilities in the magnetospheric-field configuration.
- DOI
- 10.1186/s40623-015-0335-7
- Access Restrictions
- インターネット公開
- Rights (production)
- © 2015 Uchino and Machida. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
- Related Material (URI)
- References
- A synthesis of magnetospheric substorm modelsCurrent disruption in the Earth's magnetosphere: Observations and modelsBursty bulk flows and dipolarization in MHD simulations of magnetotail reconnectionParticle simulation of magnetic reconnection in the magnetotail configurationLinear theory of anisotropy driven modes in a Harris neutral sheetA state‐of‐the‐art picture of substorm‐associated evolution of the near‐Earth magnetotail obtained from superposed epoch analysisStatistical visualization of the Earth's magnetotail and the implied mechanism of substorm triggering based on superposed-epoch analysis of THEMIS dataParticle simulations of collisionless reconnection in magnetotail configuration including electron dynamicsStatistical visualization of the Earth's magnetotail based on Geotail data and the implied substorm modelTHEMIS observations of an earthward‐propagating dipolarization frontA model for thinning of the plasma sheetEffect of electron dynamics on collisionless reconnection in two‐dimensional magnetotail equilibriaThe diffusion region in collisionless magnetic reconnectionObservations of multiple X‐line structure in the Earth's magnetotail current sheet: A Cluster case studyMagnetospheric Equilibrium Configurations and Slow Adiabatic ConvectionTransient phenomena in the magnetotail and their relation to substormsA theory of the substorm mechanismOnset of collisionless magnetic reconnection in two-dimensional current sheets and formation of dipolarization frontsCollisionless reconnection in two‐dimensional magnetotail equilibriadoes ion tearing exist?High‐speed ion flow, substorm current wedge, and multiple Pi 2 pulsationsThe development of the auroral substormInstability of the current sheet in the Earth's magnetotail with normal magnetic fieldTearing mode in thin current sheets of the Earth’s magnetosphere: A scenario of transition to unstable stateOnset of reconnection in the near magnetotail: PIC simulationsNeutral line model of substorms: Past results and present viewCollisionless reconnection supported by nongyrotropic pressure effects in hybrid and particle simulationsGeospace Environmental Modeling (GEM) Magnetic Reconnection Challenge
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 学術機関リポジトリデータベース雑誌記事索引データベースCrossref科学研究費助成事業データベース科学研究費助成事業データベース
- Bibliographic ID (NDL)
- 9534538