Density and temperature of energetic electrons in the Earth's magnetotail derived from high-latitude GPS observations during the declining phase of the solar cycle

Single relativistic-Maxwellian fits are made to high-latitude GPS-satellite observations of energetic electrons for the period January 2006–November 2010; a constellation of 12 GPS space vehicles provides the observations. The derived fit parameters (for energies ~0.1–1.0 MeV), in combination wi...

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Main Authors: M. H. Denton, T. E. Cayton
Format: Article
Language:English
Published: Copernicus Publications 2011-10-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/29/1755/2011/angeo-29-1755-2011.pdf
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author M. H. Denton
T. E. Cayton
author_facet M. H. Denton
T. E. Cayton
author_sort M. H. Denton
collection DOAJ
description Single relativistic-Maxwellian fits are made to high-latitude GPS-satellite observations of energetic electrons for the period January 2006–November 2010; a constellation of 12 GPS space vehicles provides the observations. The derived fit parameters (for energies ~0.1–1.0 MeV), in combination with field-line mapping on the nightside of the magnetosphere, provide a survey of the energetic electron density and temperature distribution in the magnetotail between McIlwain L-values of <I>L</I>=6 and <I>L</I>=22. Analysis reveals the characteristics of the density-temperature distribution of energetic electrons and its variation as a function of solar wind speed and the Kp index. The density-temperature characteristics of the magnetotail energetic electrons are very similar to those found in the outer electron radiation belt as measured at geosynchronous orbit. The energetic electron density in the magnetotail is much greater during increased geomagnetic activity and during fast solar wind. The total electron density in the magnetotail is found to be strongly correlated with solar wind speed and is at least a factor of two greater for high-speed solar wind (<I>V</I><sub>SW</sub>=500–1000 km s<sup>−1</sup>) compared to low-speed solar wind (<I>V</I><sub>SW</sub>=100–400 km s<sup>−1</sup>). These results have important implications for understanding (a) how the solar wind may modulate entry into the magnetosphere during fast and slow solar wind, and (b) if the magnetotail is a source or a sink for the outer electron radiation belt.
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spelling doaj.art-0360e48c7e9f46e4bdcc7f89d07b5bdf2022-12-22T03:23:19ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762011-10-01291755176310.5194/angeo-29-1755-2011Density and temperature of energetic electrons in the Earth's magnetotail derived from high-latitude GPS observations during the declining phase of the solar cycleM. H. Denton0T. E. Cayton1Department of Physics, Lancaster University, Lancaster, LA1 4YB, UKISR-1, Los Alamos National Laboratory, Los Alamos, NM 87545, USASingle relativistic-Maxwellian fits are made to high-latitude GPS-satellite observations of energetic electrons for the period January 2006–November 2010; a constellation of 12 GPS space vehicles provides the observations. The derived fit parameters (for energies ~0.1–1.0 MeV), in combination with field-line mapping on the nightside of the magnetosphere, provide a survey of the energetic electron density and temperature distribution in the magnetotail between McIlwain L-values of <I>L</I>=6 and <I>L</I>=22. Analysis reveals the characteristics of the density-temperature distribution of energetic electrons and its variation as a function of solar wind speed and the Kp index. The density-temperature characteristics of the magnetotail energetic electrons are very similar to those found in the outer electron radiation belt as measured at geosynchronous orbit. The energetic electron density in the magnetotail is much greater during increased geomagnetic activity and during fast solar wind. The total electron density in the magnetotail is found to be strongly correlated with solar wind speed and is at least a factor of two greater for high-speed solar wind (<I>V</I><sub>SW</sub>=500–1000 km s<sup>−1</sup>) compared to low-speed solar wind (<I>V</I><sub>SW</sub>=100–400 km s<sup>−1</sup>). These results have important implications for understanding (a) how the solar wind may modulate entry into the magnetosphere during fast and slow solar wind, and (b) if the magnetotail is a source or a sink for the outer electron radiation belt.https://www.ann-geophys.net/29/1755/2011/angeo-29-1755-2011.pdf
spellingShingle M. H. Denton
T. E. Cayton
Density and temperature of energetic electrons in the Earth's magnetotail derived from high-latitude GPS observations during the declining phase of the solar cycle
Annales Geophysicae
title Density and temperature of energetic electrons in the Earth's magnetotail derived from high-latitude GPS observations during the declining phase of the solar cycle
title_full Density and temperature of energetic electrons in the Earth's magnetotail derived from high-latitude GPS observations during the declining phase of the solar cycle
title_fullStr Density and temperature of energetic electrons in the Earth's magnetotail derived from high-latitude GPS observations during the declining phase of the solar cycle
title_full_unstemmed Density and temperature of energetic electrons in the Earth's magnetotail derived from high-latitude GPS observations during the declining phase of the solar cycle
title_short Density and temperature of energetic electrons in the Earth's magnetotail derived from high-latitude GPS observations during the declining phase of the solar cycle
title_sort density and temperature of energetic electrons in the earth s magnetotail derived from high latitude gps observations during the declining phase of the solar cycle
url https://www.ann-geophys.net/29/1755/2011/angeo-29-1755-2011.pdf
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AT tecayton densityandtemperatureofenergeticelectronsintheearthsmagnetotailderivedfromhighlatitudegpsobservationsduringthedecliningphaseofthesolarcycle