Cluster observations of surface waves on the dawn flank magnetopause

On 14 June 2001 the four Cluster spacecraft recorded multiple encounters of the dawn-side flank magnetopause. The characteristics of the observed electron populations varied between a cold, dense magnetosheath population and warmer, more rarified boundary layer population on a quasi-periodic basi...

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Main Authors: C. J. Owen, M. G. G. T. Taylor, I. C. Krauklis, A. N. Fazakerley, M. W. Dunlop, J. M. Bosqued
Format: Article
Language:English
Published: Copernicus Publications 2004-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/22/971/2004/angeo-22-971-2004.pdf
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spelling doaj-c0381ef1db0f4bc8956f4b5e447a0e2f2020-11-24T23:13:28ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762004-03-012297198310.5194/angeo-22-971-2004Cluster observations of surface waves on the dawn flank magnetopauseC. J. Owen0M. G. G. T. Taylor1M. G. G. T. Taylor2I. C. Krauklis3A. N. Fazakerley4M. W. Dunlop5M. W. Dunlop6J. M. Bosqued7Mullard Space Science Laboratory, Department of Space and Climate Physics, University College London, Holmbury St. Mary, Dorking, Surrey, RH5 6NT, UKNow at Los Alamos National Laboratory, Los Alamos, NM, USAMullard Space Science Laboratory, Department of Space and Climate Physics, University College London, Holmbury St. Mary, Dorking, Surrey, RH5 6NT, UKMullard Space Science Laboratory, Department of Space and Climate Physics, University College London, Holmbury St. Mary, Dorking, Surrey, RH5 6NT, UKMullard Space Science Laboratory, Department of Space and Climate Physics, University College London, Holmbury St. Mary, Dorking, Surrey, RH5 6NT, UKBlackett Laboratory, Imperial College of Science Technology and Medicine, Prince Consort Road, London, SW7 2BZ, UKNow at Rutherford Appleton Laboratory, Didcot, Oxon, UKCESR/CNRS, BP 4346 9, Avenue Colonel Roche, 31028 Toulouse Cedex, FranceOn 14 June 2001 the four Cluster spacecraft recorded multiple encounters of the dawn-side flank magnetopause. The characteristics of the observed electron populations varied between a cold, dense magnetosheath population and warmer, more rarified boundary layer population on a quasi-periodic basis. The demarcation between these two populations can be readily identified by gradients in the scalar temperature of the electrons. An analysis of the differences in the observed timings of the boundary at each spacecraft indicates that these magnetopause crossings are consistent with a surface wave moving across the flank magnetopause. When compared to the orientation of the magnetopause expected from models, we find that the leading edges of these waves are approximately 45° steeper than the trailing edges, consistent with the Kelvin-Helmholtz (KH) driving mechanism. A stability analysis of this interval suggests that the magnetopause is marginally stable to this mechanism during this event. Periods in which the analysis predicts that the magnetopause is unstable correspond to observations of greater wave steepening. Analysis of the pulses suggests that the waves have an average wavelength of approximately 3.4 <i>R<sub>E</sub></i> and move at an average speed of ~65km s<sup>-1</sup> in an anti-sunward and northward direction, despite the spacecraft location somewhat south of the GSE <i>Z=0</i> plane. This wave propagation direction lies close to perpendicular to the average magnetic field direction in the external magnetosheath, suggesting that these waves may preferentially propagate in the direction that requires no bending of these external field lines<br><br> <b>Key words.</b> Magnetospheric physics (magnetospheric configuration and dynamics; MHD waves and unstabilities; solar wind-magnetosphere interactions)https://www.ann-geophys.net/22/971/2004/angeo-22-971-2004.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. J. Owen
M. G. G. T. Taylor
M. G. G. T. Taylor
I. C. Krauklis
A. N. Fazakerley
M. W. Dunlop
M. W. Dunlop
J. M. Bosqued
spellingShingle C. J. Owen
M. G. G. T. Taylor
M. G. G. T. Taylor
I. C. Krauklis
A. N. Fazakerley
M. W. Dunlop
M. W. Dunlop
J. M. Bosqued
Cluster observations of surface waves on the dawn flank magnetopause
Annales Geophysicae
author_facet C. J. Owen
M. G. G. T. Taylor
M. G. G. T. Taylor
I. C. Krauklis
A. N. Fazakerley
M. W. Dunlop
M. W. Dunlop
J. M. Bosqued
author_sort C. J. Owen
title Cluster observations of surface waves on the dawn flank magnetopause
title_short Cluster observations of surface waves on the dawn flank magnetopause
title_full Cluster observations of surface waves on the dawn flank magnetopause
title_fullStr Cluster observations of surface waves on the dawn flank magnetopause
title_full_unstemmed Cluster observations of surface waves on the dawn flank magnetopause
title_sort cluster observations of surface waves on the dawn flank magnetopause
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2004-03-01
description On 14 June 2001 the four Cluster spacecraft recorded multiple encounters of the dawn-side flank magnetopause. The characteristics of the observed electron populations varied between a cold, dense magnetosheath population and warmer, more rarified boundary layer population on a quasi-periodic basis. The demarcation between these two populations can be readily identified by gradients in the scalar temperature of the electrons. An analysis of the differences in the observed timings of the boundary at each spacecraft indicates that these magnetopause crossings are consistent with a surface wave moving across the flank magnetopause. When compared to the orientation of the magnetopause expected from models, we find that the leading edges of these waves are approximately 45° steeper than the trailing edges, consistent with the Kelvin-Helmholtz (KH) driving mechanism. A stability analysis of this interval suggests that the magnetopause is marginally stable to this mechanism during this event. Periods in which the analysis predicts that the magnetopause is unstable correspond to observations of greater wave steepening. Analysis of the pulses suggests that the waves have an average wavelength of approximately 3.4 <i>R<sub>E</sub></i> and move at an average speed of ~65km s<sup>-1</sup> in an anti-sunward and northward direction, despite the spacecraft location somewhat south of the GSE <i>Z=0</i> plane. This wave propagation direction lies close to perpendicular to the average magnetic field direction in the external magnetosheath, suggesting that these waves may preferentially propagate in the direction that requires no bending of these external field lines<br><br> <b>Key words.</b> Magnetospheric physics (magnetospheric configuration and dynamics; MHD waves and unstabilities; solar wind-magnetosphere interactions)
url https://www.ann-geophys.net/22/971/2004/angeo-22-971-2004.pdf
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