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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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 |
work_keys_str_mv |
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