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...

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Main Authors: Zeller, O., Bremer, J.
Format: Article in Journal/Newspaper
Language:English
Published: München : European Geopyhsical Union 2009
Subjects:
Online Access:https://oa.tib.eu/renate/handle/123456789/4043
https://doi.org/10.34657/1678
id fttibhannoverren:oai:oa.tib.eu:123456789/4043
record_format openpolar
spelling fttibhannoverren:oai:oa.tib.eu:123456789/4043 2024-09-15T17:39:23+00:00 The influence of geomagnetic activity on mesospheric summer echoes in middle and polar latitudes Zeller, O. Bremer, J. 2009 application/pdf https://oa.tib.eu/renate/handle/123456789/4043 https://doi.org/10.34657/1678 eng eng München : European Geopyhsical Union DOI:https://doi.org/10.5194/angeo-27-831-2009 https://doi.org/10.34657/1678 https://oa.tib.eu/renate/handle/123456789/4043 CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ frei zugänglich ddc:530 Ionosphere (Mid-latitude ionosphere Polar ionosphere) Radio science (Remote sensing) comparative study flux measurement geomagnetic field geomagnetism mesosphere polar meteorology radar status-type:publishedVersion doc-type:Article doc-type:Text 2009 fttibhannoverren https://doi.org/10.34657/167810.5194/angeo-27-831-2009 2024-06-26T23:32:42Z 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. Article in Journal/Newspaper Andenes Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover)
institution Open Polar
collection Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover)
op_collection_id fttibhannoverren
language English
topic ddc:530
Ionosphere (Mid-latitude ionosphere
Polar ionosphere) Radio science (Remote sensing)
comparative study
flux measurement
geomagnetic field
geomagnetism
mesosphere
polar meteorology
radar
spellingShingle ddc:530
Ionosphere (Mid-latitude ionosphere
Polar ionosphere) Radio science (Remote sensing)
comparative study
flux measurement
geomagnetic field
geomagnetism
mesosphere
polar meteorology
radar
Zeller, O.
Bremer, J.
The influence of geomagnetic activity on mesospheric summer echoes in middle and polar latitudes
topic_facet ddc:530
Ionosphere (Mid-latitude ionosphere
Polar ionosphere) Radio science (Remote sensing)
comparative study
flux measurement
geomagnetic field
geomagnetism
mesosphere
polar meteorology
radar
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.
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://oa.tib.eu/renate/handle/123456789/4043
https://doi.org/10.34657/1678
genre Andenes
genre_facet Andenes
op_relation DOI:https://doi.org/10.5194/angeo-27-831-2009
https://doi.org/10.34657/1678
https://oa.tib.eu/renate/handle/123456789/4043
op_rights CC BY 3.0 Unported
https://creativecommons.org/licenses/by/3.0/
frei zugänglich
op_doi https://doi.org/10.34657/167810.5194/angeo-27-831-2009
_version_ 1810479506686738432