Magnetic field disturbances in the sheath region of a super-sonic interplanetary magnetic cloud

It is well-known that interplanetary magnetic clouds can cause strong geomagnetic storms due to the high magnetic field magnitude in their interior, especially if there is a large negative <I>B<sub>z</sub></I> component present. In addition, the magnetic disturbances aroun...

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Main Authors: E. Romashets, M. Vandas, S. Poedts
Format: Article
Language:English
Published: Copernicus Publications 2008-10-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/26/3153/2008/angeo-26-3153-2008.pdf
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spelling doaj-8feb5f05f137469dbb22bca26111728e2020-11-24T22:44:52ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762008-10-01263153315810.5194/angeo-26-3153-2008Magnetic field disturbances in the sheath region of a super-sonic interplanetary magnetic cloudE. Romashets0M. Vandas1S. Poedts2Prairie View A&M University, Mail Stop 2250, P.O. Box 519, Prairie View TX 77446, USAAstronomical Institute, Academy of Sciences of the Czech Republic, Praha, Czech RepublicCenter for Plasma Astrophysics, K.U.Leuven, 200 B, 3001, Leuven, BelgiumIt is well-known that interplanetary magnetic clouds can cause strong geomagnetic storms due to the high magnetic field magnitude in their interior, especially if there is a large negative <I>B<sub>z</sub></I> component present. In addition, the magnetic disturbances around such objects can play an important role in their "geo-effectiveness". On the other hand, the magnetic and flow fields in the CME sheath region in front of the body and in the rear of the cloud are important for understanding both the dynamics and the evolution of the interplanetary cloud. The "eventual" aim of this work is to calculate the magnetic field in this CME sheath region in order to evaluate the possible geo-efficiency of the cloud in terms of the maximum |<I>B<sub>z</sub></I>|-component in this region. In this paper we assess the potential of this approach by introducing a model with a simplified geometry. We describe the magnetic field between the CME shock surface and the cloud's boundary by means of a vector potential. We also apply our model and present the magnetic field distribution in the CME sheath region in front of the body and in the rear of the cloud formed after the event of 20 November 2003.https://www.ann-geophys.net/26/3153/2008/angeo-26-3153-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. Romashets
M. Vandas
S. Poedts
spellingShingle E. Romashets
M. Vandas
S. Poedts
Magnetic field disturbances in the sheath region of a super-sonic interplanetary magnetic cloud
Annales Geophysicae
author_facet E. Romashets
M. Vandas
S. Poedts
author_sort E. Romashets
title Magnetic field disturbances in the sheath region of a super-sonic interplanetary magnetic cloud
title_short Magnetic field disturbances in the sheath region of a super-sonic interplanetary magnetic cloud
title_full Magnetic field disturbances in the sheath region of a super-sonic interplanetary magnetic cloud
title_fullStr Magnetic field disturbances in the sheath region of a super-sonic interplanetary magnetic cloud
title_full_unstemmed Magnetic field disturbances in the sheath region of a super-sonic interplanetary magnetic cloud
title_sort magnetic field disturbances in the sheath region of a super-sonic interplanetary magnetic cloud
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2008-10-01
description It is well-known that interplanetary magnetic clouds can cause strong geomagnetic storms due to the high magnetic field magnitude in their interior, especially if there is a large negative <I>B<sub>z</sub></I> component present. In addition, the magnetic disturbances around such objects can play an important role in their "geo-effectiveness". On the other hand, the magnetic and flow fields in the CME sheath region in front of the body and in the rear of the cloud are important for understanding both the dynamics and the evolution of the interplanetary cloud. The "eventual" aim of this work is to calculate the magnetic field in this CME sheath region in order to evaluate the possible geo-efficiency of the cloud in terms of the maximum |<I>B<sub>z</sub></I>|-component in this region. In this paper we assess the potential of this approach by introducing a model with a simplified geometry. We describe the magnetic field between the CME shock surface and the cloud's boundary by means of a vector potential. We also apply our model and present the magnetic field distribution in the CME sheath region in front of the body and in the rear of the cloud formed after the event of 20 November 2003.
url https://www.ann-geophys.net/26/3153/2008/angeo-26-3153-2008.pdf
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AT mvandas magneticfielddisturbancesinthesheathregionofasupersonicinterplanetarymagneticcloud
AT spoedts magneticfielddisturbancesinthesheathregionofasupersonicinterplanetarymagneticcloud
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