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巻号67
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What caused the rapid recovery of the Carrington storm?

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What caused the rapid recovery of the Carrington storm?

国立国会図書館請求記号
Z19-1414
国立国会図書館書誌ID
9483550
国立国会図書館永続的識別子
info:ndljp/pid/9483550
資料種別
記事
著者
Kunihiro Keikaほか
出版者
Springer science+business media
出版年
2015-05-08
資料形態
紙・デジタル
掲載誌名
EPS : Earth, Planets and Space 67(65)
掲載ページ
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要約等:

The geomagnetic storm during the Carrington event, which occurred on 2 September 1859, displayed extremely rapid recovery. The geomagnetic field incre...

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デジタル

資料種別
記事
著者・編者
Kunihiro Keika
Yusuke Ebihara
Ryuho 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
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
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デジタル

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.
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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.
参照
Pileup accident hypothesis of magnetic storm on 17 March 2015
Temporal Variations of the Three Geomagnetic Field Components at Colaba Observatory around the Carrington Storm in 1859
New Insights From the 2003 Halloween Storm Into the Colaba 1600 nT Magnetic Depression During the 1859 Carrington Storm
Temporal 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 line
Numerical Simulation of the Ring Current: Review
GIC observations and studies in the Hydro-Québec power system
Modeling ring current proton precipitation by electromagnetic ion cyclotron waves during the May 14–16, 1997, storm
Evaluation of the tail current contribution to <i>Dst</i>
The terrestrial ring current: Origin, formation, and decay
Modeling of 1–2 September 1859 super magnetic storm
Ring current composition and sources: An update
Dst of the Carrington storm of 1859
Influence of the solar wind dynamic pressure on the decay and injection of the ring current
Modeling the recovery phase of extreme geomagnetic storms
Continued convection and the initial recovery of <i>Dst</i>
Simulation study on fundamental properties of the storm‐time ring current
Generation of 100‐year geomagnetically induced current scenarios
Dominant 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 decay
An 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 current
Ring current decay time model during geomagnetic storms: a simple analytical approach
The role of precipitation losses in producing the rapid early recovery phase of the Great Magnetic Storm of February 1986
Ionospheric mass ejection in response to a CME
The extreme magnetic storm of 1–2 September 1859
Ring current and the magnetosphere‐ionosphere coupling during the superstorm of 20 November 2003
Effects of a high‐density plasma sheet on ring current development during the November 2–6, 1993, magnetic storm
Statistical nature of geomagnetic storms
The driving of the plasma sheet by the solar wind
Solar wind control of density and temperature in the near‐Earth plasma sheet: WIND/GEOTAIL collaboration
Magnetic storms and magnetotail currents
Relation between geomagnetic sudden impulses and solar wind pressure changes-An experimental investigation
On a curious Appearance seen in the Sun
Large‐scale, near‐field magnetic fields from external sources and the corresponding induced internal field
Hyperbolic decay of the Dst Index during the recovery phase of intense geomagnetic storms
What is a geomagnetic storm?
Turbulent loss of ring current protons
Analysis of early phase ring current recovery mechanisms during geomagnetic storms
Ring current development during the great geomagnetic storm of February 1986
Description of a Singular Appearance seen in the Sun on September 1, 1859
Historically largest geomagnetic sudden commencement (SC) since 1868
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書誌ID(NDLBibID)
9483550
NII論文ID
120005758188