Correlation between ground-based observations of substorm signatures and magnetotail dynamics

We present a substorm event study using the four Cluster spacecraft in combination with ground-based instruments, in order to perform simultaneous observations in the ionosphere and magnetotail. We show good correlation between substorm signatures on the ground and in the magnetotail, even though...

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Main Authors: E. Borälv, H. J. Opgenoorth, K. Kauristie, M. Lester, J.-M. Bosqued, J. P. Dewhurst, C. J. Owen, M. Dunlop, J. A. Slavin, A. Fazakerley, C. Perry
Format: Article
Language:English
Published: Copernicus Publications 2005-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/23/997/2005/angeo-23-997-2005.pdf
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spelling doaj-99edfd252694407da9c37259851e72082020-11-24T20:58:43ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762005-03-0123997101110.5194/angeo-23-997-2005Correlation between ground-based observations of substorm signatures and magnetotail dynamicsE. Borälv0H. J. Opgenoorth1H. J. Opgenoorth2K. Kauristie3M. Lester4J.-M. Bosqued5J. P. Dewhurst6C. J. Owen7M. Dunlop8M. Dunlop9J. A. Slavin10A. Fazakerley11C. Perry12Swedish Institute of Space Physics, Uppsala, SwedenSwedish Institute of Space Physics, Uppsala, SwedenEuropean Space Agency, ESTEC, Noordwijk, NetherlandsFinnish Meteorological Institute, Space Research, Helsinki, FinlandUniversity of Leicester, Department of Physics and Astronomy, Leicester, UKCentre d’Etude Spatiale des Rayonnements, Toulouse, FranceMullard Space Science Laboratory, University College London, Surrey, UKMullard Space Science Laboratory, University College London, Surrey, UKSpace and Atmospheric Physics, Blackett Laboratory, Imperial College, London, UKSpace Science Department, Rutherford Appleton Laboratory, Oxfordshire, UKNASA Goddard Space Flight Center, Laboratory for Extraterrestrial Physics, Maryland, USAMullard Space Science Laboratory, University College London, Surrey, UKSpace Science Department, Rutherford Appleton Laboratory, Oxfordshire, UKWe present a substorm event study using the four Cluster spacecraft in combination with ground-based instruments, in order to perform simultaneous observations in the ionosphere and magnetotail. We show good correlation between substorm signatures on the ground and in the magnetotail, even though data from the northern-ground and southern-tail hemispheres are compared. During this event ground-based magnetometers show a substorm onset over Scandinavia in the pre-midnight sector. Within 1.5h the onset and three intensifications are apparent in the magnetograms. For all the substorm signatures seen on the ground, corresponding plasma sheet boundary motion is visible at Cluster, located at a downtail distance of 18.5 <i>R<sub>E</sub></i>. As a result of the substorm onset and intensifications, Cluster moves in and out between the southern plasma sheet and lobe. Due to the lack of an apparent solar wind driver and the good correlation between substorm signatures on the ground, we conclude the substorm itself is the driver for these plasma sheet dynamics. We show that in the scales of Cluster inter-spacecraft distances (~0.5 <i>R<sub>E</sub></i>) the inferred plasma sheet motion is often directed in both Y<sub>gsm</sub>- and Z<sub>gsm</sub>-directions, and discuss this finding in the context of previous studies of tail flapping and plasma sheet thickness variations.https://www.ann-geophys.net/23/997/2005/angeo-23-997-2005.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. Borälv
H. J. Opgenoorth
H. J. Opgenoorth
K. Kauristie
M. Lester
J.-M. Bosqued
J. P. Dewhurst
C. J. Owen
M. Dunlop
M. Dunlop
J. A. Slavin
A. Fazakerley
C. Perry
spellingShingle E. Borälv
H. J. Opgenoorth
H. J. Opgenoorth
K. Kauristie
M. Lester
J.-M. Bosqued
J. P. Dewhurst
C. J. Owen
M. Dunlop
M. Dunlop
J. A. Slavin
A. Fazakerley
C. Perry
Correlation between ground-based observations of substorm signatures and magnetotail dynamics
Annales Geophysicae
author_facet E. Borälv
H. J. Opgenoorth
H. J. Opgenoorth
K. Kauristie
M. Lester
J.-M. Bosqued
J. P. Dewhurst
C. J. Owen
M. Dunlop
M. Dunlop
J. A. Slavin
A. Fazakerley
C. Perry
author_sort E. Borälv
title Correlation between ground-based observations of substorm signatures and magnetotail dynamics
title_short Correlation between ground-based observations of substorm signatures and magnetotail dynamics
title_full Correlation between ground-based observations of substorm signatures and magnetotail dynamics
title_fullStr Correlation between ground-based observations of substorm signatures and magnetotail dynamics
title_full_unstemmed Correlation between ground-based observations of substorm signatures and magnetotail dynamics
title_sort correlation between ground-based observations of substorm signatures and magnetotail dynamics
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2005-03-01
description We present a substorm event study using the four Cluster spacecraft in combination with ground-based instruments, in order to perform simultaneous observations in the ionosphere and magnetotail. We show good correlation between substorm signatures on the ground and in the magnetotail, even though data from the northern-ground and southern-tail hemispheres are compared. During this event ground-based magnetometers show a substorm onset over Scandinavia in the pre-midnight sector. Within 1.5h the onset and three intensifications are apparent in the magnetograms. For all the substorm signatures seen on the ground, corresponding plasma sheet boundary motion is visible at Cluster, located at a downtail distance of 18.5 <i>R<sub>E</sub></i>. As a result of the substorm onset and intensifications, Cluster moves in and out between the southern plasma sheet and lobe. Due to the lack of an apparent solar wind driver and the good correlation between substorm signatures on the ground, we conclude the substorm itself is the driver for these plasma sheet dynamics. We show that in the scales of Cluster inter-spacecraft distances (~0.5 <i>R<sub>E</sub></i>) the inferred plasma sheet motion is often directed in both Y<sub>gsm</sub>- and Z<sub>gsm</sub>-directions, and discuss this finding in the context of previous studies of tail flapping and plasma sheet thickness variations.
url https://www.ann-geophys.net/23/997/2005/angeo-23-997-2005.pdf
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