Effect of suprathermal electrons on the intensity and Doppler frequency of electron plasma lines

In an incoherent scattering radar experiment, the spectral measurement of the so-called up- and downshifted electron plasma lines provides information about their intensity and their Doppler frequency. These two spectral lines correspond, in the backscatter geometry, to two Langmuir waves travelling...

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Published in:Annales Geophysicae
Main Authors: Guio, P., Lilensten, J.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.1007/s00585-999-0903-x
https://angeo.copernicus.org/articles/17/903/1999/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo34413 2023-05-15T16:04:48+02:00 Effect of suprathermal electrons on the intensity and Doppler frequency of electron plasma lines Guio, P. Lilensten, J. 2018-09-27 application/pdf https://doi.org/10.1007/s00585-999-0903-x https://angeo.copernicus.org/articles/17/903/1999/ eng eng doi:10.1007/s00585-999-0903-x https://angeo.copernicus.org/articles/17/903/1999/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.1007/s00585-999-0903-x 2020-07-20T16:28:02Z In an incoherent scattering radar experiment, the spectral measurement of the so-called up- and downshifted electron plasma lines provides information about their intensity and their Doppler frequency. These two spectral lines correspond, in the backscatter geometry, to two Langmuir waves travelling towards and away from the radar. In the daytime ionosphere, the presence of a small percentage of photoelectrons produced by the solar EUV of the total electron population can excite or damp these Langmuir waves above the thermal equilibrium, resulting in an enhancement of the intensity of the lines above the thermal level. The presence of photo-electrons also modifies the dielectric response function of the plasma from the Maxwellian and thus influences the Doppler frequency of the plasma lines. In this paper, we present a high time-resolution plasma-line data set collected on the Eiscat VHF radar. The analysed data are compared with a model that includes the effect of a suprathermal electron population calculated by a transport code. By comparing the intensity of the analysed plasma lines data to our model, we show that two sharp peaks in the electron suprathermal distribution in the energy range 20-30 eV causes an increased Landau damping around 24.25 eV and 26.25 eV. We have identified these two sharp peaks as the effect of the photoionisation of N 2 and O by the intense flux of monochromatic HeII radiation of wavelength 30.378 nm (40.812 eV) created in the chromospheric network and coronal holes. Furthermore, we see that what would have been interpreted as a mean Doppler drift velocity for a Maxwellian plasma is actually a shift of the Doppler frequency of the plasma lines due to suprathermal electrons. Key words. Ionosphere (electric fields and currents; solar radiation and cosmic ray effects) Text EISCAT Copernicus Publications: E-Journals Langmuir ENVELOPE(-67.150,-67.150,-66.967,-66.967) Annales Geophysicae 17 7 903 912
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description In an incoherent scattering radar experiment, the spectral measurement of the so-called up- and downshifted electron plasma lines provides information about their intensity and their Doppler frequency. These two spectral lines correspond, in the backscatter geometry, to two Langmuir waves travelling towards and away from the radar. In the daytime ionosphere, the presence of a small percentage of photoelectrons produced by the solar EUV of the total electron population can excite or damp these Langmuir waves above the thermal equilibrium, resulting in an enhancement of the intensity of the lines above the thermal level. The presence of photo-electrons also modifies the dielectric response function of the plasma from the Maxwellian and thus influences the Doppler frequency of the plasma lines. In this paper, we present a high time-resolution plasma-line data set collected on the Eiscat VHF radar. The analysed data are compared with a model that includes the effect of a suprathermal electron population calculated by a transport code. By comparing the intensity of the analysed plasma lines data to our model, we show that two sharp peaks in the electron suprathermal distribution in the energy range 20-30 eV causes an increased Landau damping around 24.25 eV and 26.25 eV. We have identified these two sharp peaks as the effect of the photoionisation of N 2 and O by the intense flux of monochromatic HeII radiation of wavelength 30.378 nm (40.812 eV) created in the chromospheric network and coronal holes. Furthermore, we see that what would have been interpreted as a mean Doppler drift velocity for a Maxwellian plasma is actually a shift of the Doppler frequency of the plasma lines due to suprathermal electrons. Key words. Ionosphere (electric fields and currents; solar radiation and cosmic ray effects)
format Text
author Guio, P.
Lilensten, J.
spellingShingle Guio, P.
Lilensten, J.
Effect of suprathermal electrons on the intensity and Doppler frequency of electron plasma lines
author_facet Guio, P.
Lilensten, J.
author_sort Guio, P.
title Effect of suprathermal electrons on the intensity and Doppler frequency of electron plasma lines
title_short Effect of suprathermal electrons on the intensity and Doppler frequency of electron plasma lines
title_full Effect of suprathermal electrons on the intensity and Doppler frequency of electron plasma lines
title_fullStr Effect of suprathermal electrons on the intensity and Doppler frequency of electron plasma lines
title_full_unstemmed Effect of suprathermal electrons on the intensity and Doppler frequency of electron plasma lines
title_sort effect of suprathermal electrons on the intensity and doppler frequency of electron plasma lines
publishDate 2018
url https://doi.org/10.1007/s00585-999-0903-x
https://angeo.copernicus.org/articles/17/903/1999/
long_lat ENVELOPE(-67.150,-67.150,-66.967,-66.967)
geographic Langmuir
geographic_facet Langmuir
genre EISCAT
genre_facet EISCAT
op_source eISSN: 1432-0576
op_relation doi:10.1007/s00585-999-0903-x
https://angeo.copernicus.org/articles/17/903/1999/
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container_title Annales Geophysicae
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