Cosmic radio noise absorption events associated with equatorward drifting arcs during a substorm growth phase

Cosmic radio noise absorption (CNA) events associated with equatorward drifting arcs during a substorm growth phase are studied by using simultaneous optical auroral, IRIS imaging riometer and EISCAT incoherent scatter radar measurements. The CNA is generally attributed to energetic particle precipi...

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Published in:Annales Geophysicae
Main Authors: J. R. T. Jussila, A. T. Aikio, S. Shalimov, S. R. Marple
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2004
Subjects:
Q
Online Access:https://doi.org/10.5194/angeo-22-1675-2004
https://doaj.org/article/a15260aeb5b54cb5990cf57122d454ba
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spelling ftdoajarticles:oai:doaj.org/article:a15260aeb5b54cb5990cf57122d454ba 2023-05-15T16:04:46+02:00 Cosmic radio noise absorption events associated with equatorward drifting arcs during a substorm growth phase J. R. T. Jussila A. T. Aikio S. Shalimov S. R. Marple 2004-04-01T00:00:00Z https://doi.org/10.5194/angeo-22-1675-2004 https://doaj.org/article/a15260aeb5b54cb5990cf57122d454ba EN eng Copernicus Publications https://www.ann-geophys.net/22/1675/2004/angeo-22-1675-2004.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-22-1675-2004 0992-7689 1432-0576 https://doaj.org/article/a15260aeb5b54cb5990cf57122d454ba Annales Geophysicae, Vol 22, Pp 1675-1686 (2004) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2004 ftdoajarticles https://doi.org/10.5194/angeo-22-1675-2004 2022-12-31T00:36:44Z Cosmic radio noise absorption (CNA) events associated with equatorward drifting arcs during a substorm growth phase are studied by using simultaneous optical auroral, IRIS imaging riometer and EISCAT incoherent scatter radar measurements. The CNA is generally attributed to energetic particle precipitation in the D-region. However, it has been argued that plasma irregularities or enhanced electron temperature ( T e ) in the E-region could also produce CNA. Both of the latter mechanisms are related to intense electric fields in the ionosphere. We present two events which occur during a substorm growth phase in the evening MLT sector. In both of the events, an auroral arc is drifting equatorward, together with a region of CNA (auroral absorption bay) located on the equatorward side and outside of the arc. Both of the events are associated with enhanced D-region electron density on the equatorward side of the auroral arc, but in the second event, a region of intense electric field and enhanced electron temperature in the E-region is also located on the equatorward side of the arc. We show that in the studied events neither plasma instabilities nor enhanced T e play a significant role in producing the measured CNA, but the CNA in the vicinity of the equatorward drifting arcs is produced by D-region energetic electron precipitation. Key words. Ionosphere (auroral ionosphere; particle precipitation; electric fields and currents) Article in Journal/Newspaper EISCAT Directory of Open Access Journals: DOAJ Articles Annales Geophysicae 22 5 1675 1686
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
spellingShingle Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
J. R. T. Jussila
A. T. Aikio
S. Shalimov
S. R. Marple
Cosmic radio noise absorption events associated with equatorward drifting arcs during a substorm growth phase
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
description Cosmic radio noise absorption (CNA) events associated with equatorward drifting arcs during a substorm growth phase are studied by using simultaneous optical auroral, IRIS imaging riometer and EISCAT incoherent scatter radar measurements. The CNA is generally attributed to energetic particle precipitation in the D-region. However, it has been argued that plasma irregularities or enhanced electron temperature ( T e ) in the E-region could also produce CNA. Both of the latter mechanisms are related to intense electric fields in the ionosphere. We present two events which occur during a substorm growth phase in the evening MLT sector. In both of the events, an auroral arc is drifting equatorward, together with a region of CNA (auroral absorption bay) located on the equatorward side and outside of the arc. Both of the events are associated with enhanced D-region electron density on the equatorward side of the auroral arc, but in the second event, a region of intense electric field and enhanced electron temperature in the E-region is also located on the equatorward side of the arc. We show that in the studied events neither plasma instabilities nor enhanced T e play a significant role in producing the measured CNA, but the CNA in the vicinity of the equatorward drifting arcs is produced by D-region energetic electron precipitation. Key words. Ionosphere (auroral ionosphere; particle precipitation; electric fields and currents)
format Article in Journal/Newspaper
author J. R. T. Jussila
A. T. Aikio
S. Shalimov
S. R. Marple
author_facet J. R. T. Jussila
A. T. Aikio
S. Shalimov
S. R. Marple
author_sort J. R. T. Jussila
title Cosmic radio noise absorption events associated with equatorward drifting arcs during a substorm growth phase
title_short Cosmic radio noise absorption events associated with equatorward drifting arcs during a substorm growth phase
title_full Cosmic radio noise absorption events associated with equatorward drifting arcs during a substorm growth phase
title_fullStr Cosmic radio noise absorption events associated with equatorward drifting arcs during a substorm growth phase
title_full_unstemmed Cosmic radio noise absorption events associated with equatorward drifting arcs during a substorm growth phase
title_sort cosmic radio noise absorption events associated with equatorward drifting arcs during a substorm growth phase
publisher Copernicus Publications
publishDate 2004
url https://doi.org/10.5194/angeo-22-1675-2004
https://doaj.org/article/a15260aeb5b54cb5990cf57122d454ba
genre EISCAT
genre_facet EISCAT
op_source Annales Geophysicae, Vol 22, Pp 1675-1686 (2004)
op_relation https://www.ann-geophys.net/22/1675/2004/angeo-22-1675-2004.pdf
https://doaj.org/toc/0992-7689
https://doaj.org/toc/1432-0576
doi:10.5194/angeo-22-1675-2004
0992-7689
1432-0576
https://doaj.org/article/a15260aeb5b54cb5990cf57122d454ba
op_doi https://doi.org/10.5194/angeo-22-1675-2004
container_title Annales Geophysicae
container_volume 22
container_issue 5
container_start_page 1675
op_container_end_page 1686
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