Space weather effects on radio propagation: study of the CEDAR, GEM and ISTP storm events

The impact of 14 geomagnetic storms from a list of CEDAR, GEM and ISTP storms, that occurred during 1997–1999, on radio propagation conditions has been investigated. The propagation conditions were estimated through variations of the MOF and LOF (the maximum and lowest operation frequencies) on thre...

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Published in:Annales Geophysicae
Main Authors: Blagoveshchensky, D. V., Kalishin, A. S., Sergeyeva, M. A.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-26-1479-2008
https://angeo.copernicus.org/articles/26/1479/2008/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo36419 2023-05-15T17:40:33+02:00 Space weather effects on radio propagation: study of the CEDAR, GEM and ISTP storm events Blagoveshchensky, D. V. Kalishin, A. S. Sergeyeva, M. A. 2018-09-27 application/pdf https://doi.org/10.5194/angeo-26-1479-2008 https://angeo.copernicus.org/articles/26/1479/2008/ eng eng doi:10.5194/angeo-26-1479-2008 https://angeo.copernicus.org/articles/26/1479/2008/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.5194/angeo-26-1479-2008 2020-07-20T16:26:54Z The impact of 14 geomagnetic storms from a list of CEDAR, GEM and ISTP storms, that occurred during 1997–1999, on radio propagation conditions has been investigated. The propagation conditions were estimated through variations of the MOF and LOF (the maximum and lowest operation frequencies) on three high-latitude HF radio paths in north-west Russia. Geophysical data of D st , B z , AE as well as some riometer data from Sodankyla observatory, Finland, were used for the analysis. It was shown that the storm impact on the ionosphere and radio propagation for each storm has an individual character. Nevertheless, there are common patterns in variation of the propagation parameters for all storms. Thus, the frequency range Δ=MOF−LOF increases several hours before a storm, then it narrows sharply during the storm, and expands again several hours after the end of the storm. This regular behaviour should be useful for the HF radio propagation predictions and frequency management at high latitudes. On the trans-auroral radio path, the time interval when the signal is lost through a storm ( t des ) depends on the local time. For the day-time storms an average value t des is 6 h, but for night storms t des is only 2 h. The ionization increase in the F2 layer before storm onset is 3.5 h during the day-time and 2.4 h at night. Mechanisms to explain the observed variations are discussed including some novel possibilities involving energy input through the cusp. Text North-West Russia Copernicus Publications: E-Journals Annales Geophysicae 26 6 1479 1490
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The impact of 14 geomagnetic storms from a list of CEDAR, GEM and ISTP storms, that occurred during 1997–1999, on radio propagation conditions has been investigated. The propagation conditions were estimated through variations of the MOF and LOF (the maximum and lowest operation frequencies) on three high-latitude HF radio paths in north-west Russia. Geophysical data of D st , B z , AE as well as some riometer data from Sodankyla observatory, Finland, were used for the analysis. It was shown that the storm impact on the ionosphere and radio propagation for each storm has an individual character. Nevertheless, there are common patterns in variation of the propagation parameters for all storms. Thus, the frequency range Δ=MOF−LOF increases several hours before a storm, then it narrows sharply during the storm, and expands again several hours after the end of the storm. This regular behaviour should be useful for the HF radio propagation predictions and frequency management at high latitudes. On the trans-auroral radio path, the time interval when the signal is lost through a storm ( t des ) depends on the local time. For the day-time storms an average value t des is 6 h, but for night storms t des is only 2 h. The ionization increase in the F2 layer before storm onset is 3.5 h during the day-time and 2.4 h at night. Mechanisms to explain the observed variations are discussed including some novel possibilities involving energy input through the cusp.
format Text
author Blagoveshchensky, D. V.
Kalishin, A. S.
Sergeyeva, M. A.
spellingShingle Blagoveshchensky, D. V.
Kalishin, A. S.
Sergeyeva, M. A.
Space weather effects on radio propagation: study of the CEDAR, GEM and ISTP storm events
author_facet Blagoveshchensky, D. V.
Kalishin, A. S.
Sergeyeva, M. A.
author_sort Blagoveshchensky, D. V.
title Space weather effects on radio propagation: study of the CEDAR, GEM and ISTP storm events
title_short Space weather effects on radio propagation: study of the CEDAR, GEM and ISTP storm events
title_full Space weather effects on radio propagation: study of the CEDAR, GEM and ISTP storm events
title_fullStr Space weather effects on radio propagation: study of the CEDAR, GEM and ISTP storm events
title_full_unstemmed Space weather effects on radio propagation: study of the CEDAR, GEM and ISTP storm events
title_sort space weather effects on radio propagation: study of the cedar, gem and istp storm events
publishDate 2018
url https://doi.org/10.5194/angeo-26-1479-2008
https://angeo.copernicus.org/articles/26/1479/2008/
genre North-West Russia
genre_facet North-West Russia
op_source eISSN: 1432-0576
op_relation doi:10.5194/angeo-26-1479-2008
https://angeo.copernicus.org/articles/26/1479/2008/
op_doi https://doi.org/10.5194/angeo-26-1479-2008
container_title Annales Geophysicae
container_volume 26
container_issue 6
container_start_page 1479
op_container_end_page 1490
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