Plasma Wave Heating in the E-region

It has been shown in previous studies that at 110 km altitude, the electron temperature can be quite large in the presence of strong electric fields. This thesis explores the possibility of deviations from the normal trends in the high latitude E-region electron heating in reaction to strong electri...

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Other Authors: St. Maurice, Jean-Pierre
Language:English
Published: 2015
Subjects:
Online Access:http://hdl.handle.net/10388/ETD-2015-01-1959
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spelling ndltd-USASK-oai-ecommons.usask.ca-10388-ETD-2015-01-19592015-03-19T12:59:43ZPlasma Wave Heating in the E-regionE-regionEISCAT UHF RadarElectron TemperatureIon TemperatureElectric FieldHeatingIt has been shown in previous studies that at 110 km altitude, the electron temperature can be quite large in the presence of strong electric fields. This thesis explores the possibility of deviations from the normal trends in the high latitude E-region electron heating in reaction to strong electric fields. The study is based on data from the EISCAT Incoherent Scatter Radar during the International Polar Year. Out of a large number of possibilities (the radar operated essentially on a continuous basis for a year) only seven events proved to have sufficiently strong electric fields and large enough plasma densities to be characterized as ‘good heating events’. The electron temperature enhancements in these events, at 110 km, were several hundred K above from the background temperature and correlated well with ion temperature at 150 km altitude. The results for these good events agreed very well with past studies, aside from the smaller starting temperatures which were likely connected to the quiet solar conditions at the time. This stated, a different type of E region electron heating event was identified. In that case the E region electron densities were small (night-time conditions free of electron precipitation) and the electron temperatures reached a maximum near 150 km altitude. In those events the electron temperature enhancements extended down to the lower altitudes, introducing small, but detectable, electron temperature enhancements all the way down to 105 km altitude. .St. Maurice, Jean-Pierre2015-03-18T12:00:11Z2015-03-18T12:00:11Z2015-012015-03-17January 2015textthesishttp://hdl.handle.net/10388/ETD-2015-01-1959eng
collection NDLTD
language English
sources NDLTD
topic E-region
EISCAT UHF Radar
Electron Temperature
Ion Temperature
Electric Field
Heating
spellingShingle E-region
EISCAT UHF Radar
Electron Temperature
Ion Temperature
Electric Field
Heating
Plasma Wave Heating in the E-region
description It has been shown in previous studies that at 110 km altitude, the electron temperature can be quite large in the presence of strong electric fields. This thesis explores the possibility of deviations from the normal trends in the high latitude E-region electron heating in reaction to strong electric fields. The study is based on data from the EISCAT Incoherent Scatter Radar during the International Polar Year. Out of a large number of possibilities (the radar operated essentially on a continuous basis for a year) only seven events proved to have sufficiently strong electric fields and large enough plasma densities to be characterized as ‘good heating events’. The electron temperature enhancements in these events, at 110 km, were several hundred K above from the background temperature and correlated well with ion temperature at 150 km altitude. The results for these good events agreed very well with past studies, aside from the smaller starting temperatures which were likely connected to the quiet solar conditions at the time. This stated, a different type of E region electron heating event was identified. In that case the E region electron densities were small (night-time conditions free of electron precipitation) and the electron temperatures reached a maximum near 150 km altitude. In those events the electron temperature enhancements extended down to the lower altitudes, introducing small, but detectable, electron temperature enhancements all the way down to 105 km altitude. .
author2 St. Maurice, Jean-Pierre
author_facet St. Maurice, Jean-Pierre
title Plasma Wave Heating in the E-region
title_short Plasma Wave Heating in the E-region
title_full Plasma Wave Heating in the E-region
title_fullStr Plasma Wave Heating in the E-region
title_full_unstemmed Plasma Wave Heating in the E-region
title_sort plasma wave heating in the e-region
publishDate 2015
url http://hdl.handle.net/10388/ETD-2015-01-1959
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