New plasmapause model derived from CHAMP field-aligned current signatures

We introduce a new model for the plasmapause location in the equatorial plane. The determination of the <I>L</I>-shell bounding the plasmasphere is based on magnetic field observations made by the CHAMP satellite in the topside ionosphere. Related signals are medium-scale field-aligne...

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Main Authors: B. Heilig, H. Lühr
Format: Article
Language:English
Published: Copernicus Publications 2013-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/31/529/2013/angeo-31-529-2013.pdf
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spelling doaj-e4de217e3c614864a27ed26eaed129342020-11-24T21:32:25ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762013-03-013152953910.5194/angeo-31-529-2013New plasmapause model derived from CHAMP field-aligned current signaturesB. Heilig0B. Heilig1H. Lühr2GFZ German Research Centre for Geosciences, Telegrafenberg, 1473 Potsdam, GermanyTihany Geophysical Observatory, Geological and Geophysical Institute of Hungary, Kossuth L. u. 91., 8237 Tihany, HungaryGFZ German Research Centre for Geosciences, Telegrafenberg, 1473 Potsdam, GermanyWe introduce a new model for the plasmapause location in the equatorial plane. The determination of the <I>L</I>-shell bounding the plasmasphere is based on magnetic field observations made by the CHAMP satellite in the topside ionosphere. Related signals are medium-scale field-aligned currents (MSFAC) (some 10 km scale size). The mid-latitude boundary of these MSFACs is used for determining the plasmapause. We are presenting a procedure for detecting the MSFAC boundary. Reliable <I>L</I>-values are obtained on the night side, whenever the solar zenith angle is below 90°. This means, the boundary is not determined well in the 08:00 to 16:00 magnetic local time (MLT) sector. The radial distance of the boundary is closely controlled by the magnetic activity index Kp. Over the Kp range 0 to 9, the <I>L</I>-value varies from 6 to 2 <I>R</I><sub>E</sub>. Conversely, the dependence on solar flux is insignificant. For a fixed Kp level, the obtained <I>L</I>-values of the boundary form a ring on an MLT dial plot with a centre somewhat offset from the geomagnetic pole. This Kp and local time dependent feature is used for predicting the location of the MSFAC boundary at all MLTs based on a single <I>L</I>-value determination by CHAMP. We compared the location of the MSFAC boundary during the years 2001–2002 with the <I>L</I>-value of the plasmapause, determined from in situ observations by the IMAGE spacecraft. The mean difference in radial distance is within a 1 <I>R</I><sub>E</sub> range for all local times and Kp values. The plasmapause is generally found earthward of the FAC boundary, except for the duskside. By considering this systematic displacement and by taking into account the diurnal variation and Kp-dependence of the residuals, we are able to construct an empirical model of the plasmapause location that is based on MSFAC measurements from CHAMP. Our new model PPCH-2012 agrees with IMAGE in situ observations within a standard deviation of 0.79 <I>R</I><sub>E</sub>.https://www.ann-geophys.net/31/529/2013/angeo-31-529-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author B. Heilig
B. Heilig
H. Lühr
spellingShingle B. Heilig
B. Heilig
H. Lühr
New plasmapause model derived from CHAMP field-aligned current signatures
Annales Geophysicae
author_facet B. Heilig
B. Heilig
H. Lühr
author_sort B. Heilig
title New plasmapause model derived from CHAMP field-aligned current signatures
title_short New plasmapause model derived from CHAMP field-aligned current signatures
title_full New plasmapause model derived from CHAMP field-aligned current signatures
title_fullStr New plasmapause model derived from CHAMP field-aligned current signatures
title_full_unstemmed New plasmapause model derived from CHAMP field-aligned current signatures
title_sort new plasmapause model derived from champ field-aligned current signatures
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2013-03-01
description We introduce a new model for the plasmapause location in the equatorial plane. The determination of the <I>L</I>-shell bounding the plasmasphere is based on magnetic field observations made by the CHAMP satellite in the topside ionosphere. Related signals are medium-scale field-aligned currents (MSFAC) (some 10 km scale size). The mid-latitude boundary of these MSFACs is used for determining the plasmapause. We are presenting a procedure for detecting the MSFAC boundary. Reliable <I>L</I>-values are obtained on the night side, whenever the solar zenith angle is below 90°. This means, the boundary is not determined well in the 08:00 to 16:00 magnetic local time (MLT) sector. The radial distance of the boundary is closely controlled by the magnetic activity index Kp. Over the Kp range 0 to 9, the <I>L</I>-value varies from 6 to 2 <I>R</I><sub>E</sub>. Conversely, the dependence on solar flux is insignificant. For a fixed Kp level, the obtained <I>L</I>-values of the boundary form a ring on an MLT dial plot with a centre somewhat offset from the geomagnetic pole. This Kp and local time dependent feature is used for predicting the location of the MSFAC boundary at all MLTs based on a single <I>L</I>-value determination by CHAMP. We compared the location of the MSFAC boundary during the years 2001–2002 with the <I>L</I>-value of the plasmapause, determined from in situ observations by the IMAGE spacecraft. The mean difference in radial distance is within a 1 <I>R</I><sub>E</sub> range for all local times and Kp values. The plasmapause is generally found earthward of the FAC boundary, except for the duskside. By considering this systematic displacement and by taking into account the diurnal variation and Kp-dependence of the residuals, we are able to construct an empirical model of the plasmapause location that is based on MSFAC measurements from CHAMP. Our new model PPCH-2012 agrees with IMAGE in situ observations within a standard deviation of 0.79 <I>R</I><sub>E</sub>.
url https://www.ann-geophys.net/31/529/2013/angeo-31-529-2013.pdf
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