The influence of geomagnetic activity on mesospheric summer echoes in middle and polar latitudes
The dependence of mesospheric VHF radar echoes during summer months on geomagnetic activity has been investigated with observation data of the OSWIN radar in Kühlungsborn (54° N) and of the ALWIN radar in Andenes (69° N). Using daily mean values of VHF radar echoes and of geomagnetic activity indice...
Main Authors: | , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
München : European Geopyhsical Union
2009
|
Subjects: | |
Online Access: | https://doi.org/10.34657/1678 https://oa.tib.eu/renate/handle/123456789/4043 |
id |
ftleibnizopen:oai:oai.leibnizopen.de:OdpQoYoBbHMkKcxzxhEi |
---|---|
record_format |
openpolar |
spelling |
ftleibnizopen:oai:oai.leibnizopen.de:OdpQoYoBbHMkKcxzxhEi 2023-10-09T21:44:32+02:00 The influence of geomagnetic activity on mesospheric summer echoes in middle and polar latitudes Zeller, O. Bremer, J. 2009 application/pdf https://doi.org/10.34657/1678 https://oa.tib.eu/renate/handle/123456789/4043 eng eng München : European Geopyhsical Union CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ Annales Geophysicae, Volume 27, Issue 2, Page 831-837 Ionosphere (Mid-latitude ionosphere Polar ionosphere) Radio science (Remote sensing) comparative study flux measurement geomagnetic field geomagnetism mesosphere polar meteorology radar 530 article Text 2009 ftleibnizopen https://doi.org/10.34657/1678 2023-09-17T23:35:14Z The dependence of mesospheric VHF radar echoes during summer months on geomagnetic activity has been investigated with observation data of the OSWIN radar in Kühlungsborn (54° N) and of the ALWIN radar in Andenes (69° N). Using daily mean values of VHF radar echoes and of geomagnetic activity indices in superimposed epoch analyses, the comparison of both data sets shows in general stronger radar echoes on the day of the maximum geomagnetic activity, the maximum value one day after the geomagnetic disturbance, and enhanced radar echoes also on the following 2–3 days. This phenomenon is observed at middle and polar latitudes and can be explained by precipitating particle fluxes during the ionospheric post storm effect. At polar latitudes, the radar echoes decrease however during and one day after very strong geomagnetic disturbances. The possible reason of this surprising effect is discussed. publishedVersion Article in Journal/Newspaper Andenes LeibnizOpen (The Leibniz Association) |
institution |
Open Polar |
collection |
LeibnizOpen (The Leibniz Association) |
op_collection_id |
ftleibnizopen |
language |
English |
topic |
Ionosphere (Mid-latitude ionosphere Polar ionosphere) Radio science (Remote sensing) comparative study flux measurement geomagnetic field geomagnetism mesosphere polar meteorology radar 530 |
spellingShingle |
Ionosphere (Mid-latitude ionosphere Polar ionosphere) Radio science (Remote sensing) comparative study flux measurement geomagnetic field geomagnetism mesosphere polar meteorology radar 530 Zeller, O. Bremer, J. The influence of geomagnetic activity on mesospheric summer echoes in middle and polar latitudes |
topic_facet |
Ionosphere (Mid-latitude ionosphere Polar ionosphere) Radio science (Remote sensing) comparative study flux measurement geomagnetic field geomagnetism mesosphere polar meteorology radar 530 |
description |
The dependence of mesospheric VHF radar echoes during summer months on geomagnetic activity has been investigated with observation data of the OSWIN radar in Kühlungsborn (54° N) and of the ALWIN radar in Andenes (69° N). Using daily mean values of VHF radar echoes and of geomagnetic activity indices in superimposed epoch analyses, the comparison of both data sets shows in general stronger radar echoes on the day of the maximum geomagnetic activity, the maximum value one day after the geomagnetic disturbance, and enhanced radar echoes also on the following 2–3 days. This phenomenon is observed at middle and polar latitudes and can be explained by precipitating particle fluxes during the ionospheric post storm effect. At polar latitudes, the radar echoes decrease however during and one day after very strong geomagnetic disturbances. The possible reason of this surprising effect is discussed. publishedVersion |
format |
Article in Journal/Newspaper |
author |
Zeller, O. Bremer, J. |
author_facet |
Zeller, O. Bremer, J. |
author_sort |
Zeller, O. |
title |
The influence of geomagnetic activity on mesospheric summer echoes in middle and polar latitudes |
title_short |
The influence of geomagnetic activity on mesospheric summer echoes in middle and polar latitudes |
title_full |
The influence of geomagnetic activity on mesospheric summer echoes in middle and polar latitudes |
title_fullStr |
The influence of geomagnetic activity on mesospheric summer echoes in middle and polar latitudes |
title_full_unstemmed |
The influence of geomagnetic activity on mesospheric summer echoes in middle and polar latitudes |
title_sort |
influence of geomagnetic activity on mesospheric summer echoes in middle and polar latitudes |
publisher |
München : European Geopyhsical Union |
publishDate |
2009 |
url |
https://doi.org/10.34657/1678 https://oa.tib.eu/renate/handle/123456789/4043 |
genre |
Andenes |
genre_facet |
Andenes |
op_source |
Annales Geophysicae, Volume 27, Issue 2, Page 831-837 |
op_rights |
CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ |
op_doi |
https://doi.org/10.34657/1678 |
_version_ |
1779311061979103232 |