Secondary electron emission from meteoric smoke particles inside the polar ionosphere

The charging by secondary electron emission (SEE) from particles is known as a significant charging process in astrophysical plasmas. This work aims at evaluating the significance of SEE for charging of meteoric smoke particles (MSPs) in the Earth's polar atmosphere. Here, the atmosphere is...

Full description

Bibliographic Details
Main Authors: C. Baumann, M. Rapp, A. Kero
Format: Article
Language:English
Published: Copernicus Publications 2016-06-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/34/573/2016/angeo-34-573-2016.pdf
id doaj-e73e714fd2f947a491674c631f895b6e
record_format Article
spelling doaj-e73e714fd2f947a491674c631f895b6e2020-11-24T23:01:20ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762016-06-013457358010.5194/angeo-34-573-2016Secondary electron emission from meteoric smoke particles inside the polar ionosphereC. Baumann0M. Rapp1M. Rapp2A. Kero3Deutsches Zentrum für Luft- und Raumfahrt, Institut für Physik der Atmosphäre, Oberpfaffenhofen, GermanyDeutsches Zentrum für Luft- und Raumfahrt, Institut für Physik der Atmosphäre, Oberpfaffenhofen, GermanyMeteorologisches Institut München, Ludwig-Maximilians-Universität München, Munich, GermanySodankylä Geophysical Observatory, University of Oulu, Tähteläntie 62, 99600, Sodankylä, FinlandThe charging by secondary electron emission (SEE) from particles is known as a significant charging process in astrophysical plasmas. This work aims at evaluating the significance of SEE for charging of meteoric smoke particles (MSPs) in the Earth's polar atmosphere. Here, the atmosphere is subject to a bombardment of energetic electrons from the magnetosphere (and partly the sun). We employ the SEE formalism to MSPs in the upper mesosphere using electron precipitation fluxes for three different precipitation strengths. In addition, we address the possible effect of tertiary electron emission (TEE) from MSPs induced by atmospheric secondary electrons for one precipitation case. The SEE and TEE rates from MSPs of different sizes are compared to plasma attachment and photodetachment and photoionization rates of MSPs. The needed concentration of electrons and ions have been modeled with the Sodankylä Ion and Neutral Chemistry (SIC) model with included electron precipitation spectra as an additional ionization source. We find that secondary electron emission from MSPs is not a relevant charging mechanism for MSPs. The electron attachment to MSPs and photodetachment of negatively charged MSPs are the most important processes also during energetic electron precipitation.https://www.ann-geophys.net/34/573/2016/angeo-34-573-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. Baumann
M. Rapp
M. Rapp
A. Kero
spellingShingle C. Baumann
M. Rapp
M. Rapp
A. Kero
Secondary electron emission from meteoric smoke particles inside the polar ionosphere
Annales Geophysicae
author_facet C. Baumann
M. Rapp
M. Rapp
A. Kero
author_sort C. Baumann
title Secondary electron emission from meteoric smoke particles inside the polar ionosphere
title_short Secondary electron emission from meteoric smoke particles inside the polar ionosphere
title_full Secondary electron emission from meteoric smoke particles inside the polar ionosphere
title_fullStr Secondary electron emission from meteoric smoke particles inside the polar ionosphere
title_full_unstemmed Secondary electron emission from meteoric smoke particles inside the polar ionosphere
title_sort secondary electron emission from meteoric smoke particles inside the polar ionosphere
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2016-06-01
description The charging by secondary electron emission (SEE) from particles is known as a significant charging process in astrophysical plasmas. This work aims at evaluating the significance of SEE for charging of meteoric smoke particles (MSPs) in the Earth's polar atmosphere. Here, the atmosphere is subject to a bombardment of energetic electrons from the magnetosphere (and partly the sun). We employ the SEE formalism to MSPs in the upper mesosphere using electron precipitation fluxes for three different precipitation strengths. In addition, we address the possible effect of tertiary electron emission (TEE) from MSPs induced by atmospheric secondary electrons for one precipitation case. The SEE and TEE rates from MSPs of different sizes are compared to plasma attachment and photodetachment and photoionization rates of MSPs. The needed concentration of electrons and ions have been modeled with the Sodankylä Ion and Neutral Chemistry (SIC) model with included electron precipitation spectra as an additional ionization source. We find that secondary electron emission from MSPs is not a relevant charging mechanism for MSPs. The electron attachment to MSPs and photodetachment of negatively charged MSPs are the most important processes also during energetic electron precipitation.
url https://www.ann-geophys.net/34/573/2016/angeo-34-573-2016.pdf
work_keys_str_mv AT cbaumann secondaryelectronemissionfrommeteoricsmokeparticlesinsidethepolarionosphere
AT mrapp secondaryelectronemissionfrommeteoricsmokeparticlesinsidethepolarionosphere
AT mrapp secondaryelectronemissionfrommeteoricsmokeparticlesinsidethepolarionosphere
AT akero secondaryelectronemissionfrommeteoricsmokeparticlesinsidethepolarionosphere
_version_ 1725639946393354240