What caused the rapid recovery of the Carrington storm?
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- 資料種別
- 記事
- 著者・編者
- Kunihiro KeikaYusuke EbiharaRyuho Kataoka
- 出版年月日等
- 2015-05-08
- 出版年(W3CDTF)
- 2015-05-08
- タイトル(掲載誌)
- EPS : Earth, Planets and Space
- 巻号年月日等(掲載誌)
- 67(65)
- 掲載巻
- 67(65)
- ISSN(掲載誌)
- 1880-5981
- ISSN-L(掲載誌)
- 1343-8832
- 本文の言語コード
- eng
- DOI
- 10.1186/s40623-015-0234-y
- 国立国会図書館永続的識別子
- info:ndljp/pid/9483550
- コレクション(共通)
- コレクション(障害者向け資料:レベル1)
- コレクション(個別)
- 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
- 収集根拠
- オンライン資料収集制度
- 受理日(W3CDTF)
- 2015-08-17T20:47:01+09:00
- 保存日(W3CDTF)
- 2015-06-20
- 記録形式(IMT)
- application/pdf
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
- 図書館・個人送信対象外
- 遠隔複写可否(NDL)
- 可
- 掲載誌(国立国会図書館永続的識別子)
- info:ndljp/pid/9227920
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- 要約等
- The geomagnetic storm during the Carrington event, which occurred on 2 September 1859, displayed extremely rapid recovery. The geomagnetic field increased by approximately 650 nT/h at Bombay, India, and by >300 nT/h in 1-h averaged data. Although the rapid recovery is considered due to a sudden increase in the magnetopause current, a sudden decrease of the ring current, or/and a sudden enhancement of the ionospheric currents, this study focuses on the ring current decay. The Carrington rapid recovery had a time constant (approximately 1 h) comparable to the storm development (i.e., decrease in the geomagnetic field), indicating that energy loss from the ring current region is predominantly controlled by E × B convection transport which is responsible for energy input during the storm main phase. This feature has led us to a hypothesis that the flow-out of dense ring current ions and injections of tenuous plasma sheet ions caused the rapid decay of the ring current and in turn the storm rapid recovery. This study examines whether the Carrington rapid recovery can be explained by the flow-out effect. We extend the empirical Burton’s model to a model that takes into consideration a sudden change in solar wind density which is correlated with plasma sheet density. We first apply the extended Burton’s model to previously observed four intense magnetic storms (Dst minimum < −200 nT) for which solar wind data are available. Using the best fit parameters found by forward modeling, the extended model estimates the recovery of the Carrington storm. The estimate indicates that a solar wind structure with a density bump by approximately 100 cm[−3] (and southward interplanetary magnetic field (IMF) of 65 nT and solar wind speed of 1, 500 km/s) can cause the rapid recovery under a continuous southward IMF condition. We conclude that the flow-out effect plays a significant role in producing the rapid recovery of the Carrington storm.
- DOI
- 10.1186/s40623-015-0234-y
- オンライン閲覧公開範囲
- インターネット公開
- 著作権情報
- © 2015 Keika et al.; licensee Springer. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited.
- 関連情報(URI)
- 参照
- Pileup accident hypothesis of magnetic storm on 17 March 2015Temporal Variations of the Three Geomagnetic Field Components at Colaba Observatory around the Carrington Storm in 1859New Insights From the 2003 Halloween Storm Into the Colaba 1600 nT Magnetic Depression During the 1859 Carrington StormTemporal and Spatial Evolutions of a Large Sunspot Group and Great Auroral Storms Around the Carrington Event in 1859
- 参照
- Rapid decay of storm time ring current due to pitch angle scattering in curved field lineNumerical Simulation of the Ring Current: ReviewGIC observations and studies in the Hydro-Québec power systemModeling ring current proton precipitation by electromagnetic ion cyclotron waves during the May 14–16, 1997, stormEvaluation of the tail current contribution to <i>Dst</i>The terrestrial ring current: Origin, formation, and decayModeling of 1–2 September 1859 super magnetic stormRing current composition and sources: An updateDst of the Carrington storm of 1859Influence of the solar wind dynamic pressure on the decay and injection of the ring currentModeling the recovery phase of extreme geomagnetic stormsContinued convection and the initial recovery of <i>Dst</i>Simulation study on fundamental properties of the storm‐time ring currentGeneration of 100‐year geomagnetically induced current scenariosDominant role of the asymmetric ring current in producing the stormtime <i>Dst</i>*An empirical phase space analysis of ring current dynamics: Solar wind control of injection and decayAn empirical relationship between interplanetary conditions and<i>Dst</i>Solar wind‐magnetosphere coupling during intense magnetic storms (1978‐1979)Simulations of phase space distributions of storm time proton ring currentRing current decay time model during geomagnetic storms: a simple analytical approachThe role of precipitation losses in producing the rapid early recovery phase of the Great Magnetic Storm of February 1986Ionospheric mass ejection in response to a CMEThe extreme magnetic storm of 1–2 September 1859Ring current and the magnetosphere‐ionosphere coupling during the superstorm of 20 November 2003Effects of a high‐density plasma sheet on ring current development during the November 2–6, 1993, magnetic stormStatistical nature of geomagnetic stormsThe driving of the plasma sheet by the solar windSolar wind control of density and temperature in the near‐Earth plasma sheet: WIND/GEOTAIL collaborationMagnetic storms and magnetotail currentsRelation between geomagnetic sudden impulses and solar wind pressure changes-An experimental investigationOn a curious Appearance seen in the SunLarge‐scale, near‐field magnetic fields from external sources and the corresponding induced internal fieldHyperbolic decay of the Dst Index during the recovery phase of intense geomagnetic stormsWhat is a geomagnetic storm?Turbulent loss of ring current protonsAnalysis of early phase ring current recovery mechanisms during geomagnetic stormsRing current development during the great geomagnetic storm of February 1986Description of a Singular Appearance seen in the Sun on September 1, 1859Historically largest geomagnetic sudden commencement (SC) since 1868
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 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CrossrefCiNii Articles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CrossrefCrossrefCrossrefCrossref
- 書誌ID(NDLBibID)
- 9483550
- NII論文ID
- 120005758188