Modelling of N21P emission rates in aurora using various cross sections for excitation

Measurements of N 2 1P auroral emissions from the (4,1) and (5,2) bands have been made at high temporal and spatial resolution in the region of the magnetic zenith. The instrument used was the auroral imager ASK, situated at Ramfjordmoen, Norway (69.6 N, 19.2 E) on 22 October 2006. Measurements from...

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Published in:Annales Geophysicae
Main Authors: Ashrafi, M., Lanchester, B. S., Lummerzheim, D., Ivchenko, N., Jokiaho, O.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-27-2545-2009
https://angeo.copernicus.org/articles/27/2545/2009/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo36844 2023-05-15T16:04:46+02:00 Modelling of N21P emission rates in aurora using various cross sections for excitation Ashrafi, M. Lanchester, B. S. Lummerzheim, D. Ivchenko, N. Jokiaho, O. 2018-09-27 application/pdf https://doi.org/10.5194/angeo-27-2545-2009 https://angeo.copernicus.org/articles/27/2545/2009/ eng eng doi:10.5194/angeo-27-2545-2009 https://angeo.copernicus.org/articles/27/2545/2009/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.5194/angeo-27-2545-2009 2020-07-20T16:26:38Z Measurements of N 2 1P auroral emissions from the (4,1) and (5,2) bands have been made at high temporal and spatial resolution in the region of the magnetic zenith. The instrument used was the auroral imager ASK, situated at Ramfjordmoen, Norway (69.6 N, 19.2 E) on 22 October 2006. Measurements from the European Incoherent Scatter Radar (EISCAT) have been combined with the optical measurements, and incorporated into an ionospheric model to obtain height profiles of electron density and emission rates of the N 2 1P bands. The radar data provide essential verification that the energy flux used in the model is correct. One of the most important inputs to the model is the cross section for excitation to the B 3 Π g electronic state, as well as the cross sections to higher states from which cascading into the B state occurs. The balance equations for production and loss of the populations of all levels in each state are solved in order to find the cascade contributions. Several sets of cross sections have been considered, and selected cross sections have been used to construct "emission" cross sections for the observed bands. The resulting brightnesses are compared with those measured by ASK. The importance of specific contributions from cascading is found, with more than 50% of the total brightness resulting from cascading. The cross sections used are found to produce a range of brightnesses well within the uncertainty of both the modelled and measured values. Text EISCAT Copernicus Publications: E-Journals Norway Ramfjordmoen ENVELOPE(19.207,19.207,69.584,69.584) Annales Geophysicae 27 6 2545 2553
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Measurements of N 2 1P auroral emissions from the (4,1) and (5,2) bands have been made at high temporal and spatial resolution in the region of the magnetic zenith. The instrument used was the auroral imager ASK, situated at Ramfjordmoen, Norway (69.6 N, 19.2 E) on 22 October 2006. Measurements from the European Incoherent Scatter Radar (EISCAT) have been combined with the optical measurements, and incorporated into an ionospheric model to obtain height profiles of electron density and emission rates of the N 2 1P bands. The radar data provide essential verification that the energy flux used in the model is correct. One of the most important inputs to the model is the cross section for excitation to the B 3 Π g electronic state, as well as the cross sections to higher states from which cascading into the B state occurs. The balance equations for production and loss of the populations of all levels in each state are solved in order to find the cascade contributions. Several sets of cross sections have been considered, and selected cross sections have been used to construct "emission" cross sections for the observed bands. The resulting brightnesses are compared with those measured by ASK. The importance of specific contributions from cascading is found, with more than 50% of the total brightness resulting from cascading. The cross sections used are found to produce a range of brightnesses well within the uncertainty of both the modelled and measured values.
format Text
author Ashrafi, M.
Lanchester, B. S.
Lummerzheim, D.
Ivchenko, N.
Jokiaho, O.
spellingShingle Ashrafi, M.
Lanchester, B. S.
Lummerzheim, D.
Ivchenko, N.
Jokiaho, O.
Modelling of N21P emission rates in aurora using various cross sections for excitation
author_facet Ashrafi, M.
Lanchester, B. S.
Lummerzheim, D.
Ivchenko, N.
Jokiaho, O.
author_sort Ashrafi, M.
title Modelling of N21P emission rates in aurora using various cross sections for excitation
title_short Modelling of N21P emission rates in aurora using various cross sections for excitation
title_full Modelling of N21P emission rates in aurora using various cross sections for excitation
title_fullStr Modelling of N21P emission rates in aurora using various cross sections for excitation
title_full_unstemmed Modelling of N21P emission rates in aurora using various cross sections for excitation
title_sort modelling of n21p emission rates in aurora using various cross sections for excitation
publishDate 2018
url https://doi.org/10.5194/angeo-27-2545-2009
https://angeo.copernicus.org/articles/27/2545/2009/
long_lat ENVELOPE(19.207,19.207,69.584,69.584)
geographic Norway
Ramfjordmoen
geographic_facet Norway
Ramfjordmoen
genre EISCAT
genre_facet EISCAT
op_source eISSN: 1432-0576
op_relation doi:10.5194/angeo-27-2545-2009
https://angeo.copernicus.org/articles/27/2545/2009/
op_doi https://doi.org/10.5194/angeo-27-2545-2009
container_title Annales Geophysicae
container_volume 27
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