Polar and Cluster observations of a dayside inverted-V during conjunction

We investigate particle and fields data during a conjunction of the Polar and Cluster spacecraft. This conjunction occurs near the dayside cusp boundary layer when a dayside inverted-V was observed in the particle data of both satellites. Electron, ion, electric field, and magnetic field data fr...

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Main Authors: J. D. Menietti, R. A. Frahm, A. Korth, F. S. Mozer, Y. Khotyaintsev
Format: Article
Language:English
Published: Copernicus Publications 2007-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/25/543/2007/angeo-25-543-2007.pdf
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spelling doaj-bc9c2b16fa954ef0a046fdb126b8d0492020-11-24T23:14:48ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762007-03-012554355510.5194/angeo-25-543-2007Polar and Cluster observations of a dayside inverted-V during conjunctionJ. D. Menietti0R. A. Frahm1A. Korth2F. S. Mozer3Y. Khotyaintsev4University of Iowa, Department of Physics and Astronomy, Iowa City, IA, USASouthwest Research Institute, 6220 Culebra Road, San Antonio, TX, USAMax-Planck-Institut fur Sonnensystemforschung, Katlenburg-Lindau, GermanySpace Science Lab, University of California, Berlekey, CA, USAInstitutet fur rymdfysik (IRFU), Uppsala, SwedenWe investigate particle and fields data during a conjunction of the Polar and Cluster spacecraft. This conjunction occurs near the dayside cusp boundary layer when a dayside inverted-V was observed in the particle data of both satellites. Electron, ion, electric field, and magnetic field data from each satellite confirm that the dayside inverted-V (DSIV) structure is present at the location of both satellites and the electric fields persist from the altitude of the Polar (lower) spacecraft to the altitude of the Cluster spacecraft. We observe accelerated, precipitating electrons and upward ions along the magnetic field. In addition, large amplitude electric fields perpendicular to the ambient magnetic field seen by Polar and by Cluster suggest significant parallel electric fields associated with these events. For similar DSIV events observed by the Polar spacecraft, plasma waves (identified as possible Alfvén waves) have been observed to propagate in both directions along the magnetic field line. Future conjunctions will be necessary to confirm that DSIVs are associated with reconnection sites.https://www.ann-geophys.net/25/543/2007/angeo-25-543-2007.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. D. Menietti
R. A. Frahm
A. Korth
F. S. Mozer
Y. Khotyaintsev
spellingShingle J. D. Menietti
R. A. Frahm
A. Korth
F. S. Mozer
Y. Khotyaintsev
Polar and Cluster observations of a dayside inverted-V during conjunction
Annales Geophysicae
author_facet J. D. Menietti
R. A. Frahm
A. Korth
F. S. Mozer
Y. Khotyaintsev
author_sort J. D. Menietti
title Polar and Cluster observations of a dayside inverted-V during conjunction
title_short Polar and Cluster observations of a dayside inverted-V during conjunction
title_full Polar and Cluster observations of a dayside inverted-V during conjunction
title_fullStr Polar and Cluster observations of a dayside inverted-V during conjunction
title_full_unstemmed Polar and Cluster observations of a dayside inverted-V during conjunction
title_sort polar and cluster observations of a dayside inverted-v during conjunction
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2007-03-01
description We investigate particle and fields data during a conjunction of the Polar and Cluster spacecraft. This conjunction occurs near the dayside cusp boundary layer when a dayside inverted-V was observed in the particle data of both satellites. Electron, ion, electric field, and magnetic field data from each satellite confirm that the dayside inverted-V (DSIV) structure is present at the location of both satellites and the electric fields persist from the altitude of the Polar (lower) spacecraft to the altitude of the Cluster spacecraft. We observe accelerated, precipitating electrons and upward ions along the magnetic field. In addition, large amplitude electric fields perpendicular to the ambient magnetic field seen by Polar and by Cluster suggest significant parallel electric fields associated with these events. For similar DSIV events observed by the Polar spacecraft, plasma waves (identified as possible Alfvén waves) have been observed to propagate in both directions along the magnetic field line. Future conjunctions will be necessary to confirm that DSIVs are associated with reconnection sites.
url https://www.ann-geophys.net/25/543/2007/angeo-25-543-2007.pdf
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