Occurrence of polar mesosphere summer echoes at very high latitudes

Observations of polar mesosphere summer echoes (PMSE) have been carried out during the summer periodes 1999–2001 and 2003–2004 at the very high latitude of 78° N using the SOUSY Svalbard Radar (53.5 MHz) at Longyearbyen. Although the measurements could not be done continuously in these seasons, PMSE...

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Published in:Annales Geophysicae
Main Authors: M. Zecha, J. Röttger
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2009
Subjects:
Q
Online Access:https://doi.org/10.5194/angeo-27-1331-2009
https://doaj.org/article/fefe331304544d1b82463c6c8955f399
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spelling ftdoajarticles:oai:doaj.org/article:fefe331304544d1b82463c6c8955f399 2023-05-15T17:08:31+02:00 Occurrence of polar mesosphere summer echoes at very high latitudes M. Zecha J. Röttger 2009-03-01T00:00:00Z https://doi.org/10.5194/angeo-27-1331-2009 https://doaj.org/article/fefe331304544d1b82463c6c8955f399 EN eng Copernicus Publications https://www.ann-geophys.net/27/1331/2009/angeo-27-1331-2009.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-27-1331-2009 0992-7689 1432-0576 https://doaj.org/article/fefe331304544d1b82463c6c8955f399 Annales Geophysicae, Vol 27, Pp 1331-1342 (2009) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2009 ftdoajarticles https://doi.org/10.5194/angeo-27-1331-2009 2022-12-31T06:24:29Z Observations of polar mesosphere summer echoes (PMSE) have been carried out during the summer periodes 1999–2001 and 2003–2004 at the very high latitude of 78° N using the SOUSY Svalbard Radar (53.5 MHz) at Longyearbyen. Although the measurements could not be done continuously in these seasons, PMSE have been detected over more than 6600 h of 9300 h of observation time overall. Using this data base, particular PMSE occurrence characteristics have been determined. PMSE at Svalbard appear from the middle of May to the end of August with an almost permanent total occurrence in June and July. Diurnal variations are observable in the height-depend occurrence rates and in PMSE thickness, they show a maximum around 09:00–10:00 UTC and a minimum around 21:00–22:00 UTC. PMSE occur nearly exclusively between a height of 80 km and 92 km with a maximum near 85 km. However, PMSE appear not simultaneously over the entire height range, the mean vertical PMSE extension is around 4–6 km in June and July. Furthermore, typically PMSE are separated into several layers, and only 30% of all PMSE are single layers. The probability of multiple layers is greater in June and July than at the beginning and the end of the PMSE season and shows a marked 5-day-variation. The same variation is noticeable in the seasonal dependence of the PMSE occurrence and the PMSE thickness. We finally discuss potential geophysical processes to explain our observational results. Article in Journal/Newspaper Longyearbyen Svalbard Directory of Open Access Journals: DOAJ Articles Longyearbyen Svalbard Annales Geophysicae 27 3 1331 1342
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
M. Zecha
J. Röttger
Occurrence of polar mesosphere summer echoes at very high latitudes
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
description Observations of polar mesosphere summer echoes (PMSE) have been carried out during the summer periodes 1999–2001 and 2003–2004 at the very high latitude of 78° N using the SOUSY Svalbard Radar (53.5 MHz) at Longyearbyen. Although the measurements could not be done continuously in these seasons, PMSE have been detected over more than 6600 h of 9300 h of observation time overall. Using this data base, particular PMSE occurrence characteristics have been determined. PMSE at Svalbard appear from the middle of May to the end of August with an almost permanent total occurrence in June and July. Diurnal variations are observable in the height-depend occurrence rates and in PMSE thickness, they show a maximum around 09:00–10:00 UTC and a minimum around 21:00–22:00 UTC. PMSE occur nearly exclusively between a height of 80 km and 92 km with a maximum near 85 km. However, PMSE appear not simultaneously over the entire height range, the mean vertical PMSE extension is around 4–6 km in June and July. Furthermore, typically PMSE are separated into several layers, and only 30% of all PMSE are single layers. The probability of multiple layers is greater in June and July than at the beginning and the end of the PMSE season and shows a marked 5-day-variation. The same variation is noticeable in the seasonal dependence of the PMSE occurrence and the PMSE thickness. We finally discuss potential geophysical processes to explain our observational results.
format Article in Journal/Newspaper
author M. Zecha
J. Röttger
author_facet M. Zecha
J. Röttger
author_sort M. Zecha
title Occurrence of polar mesosphere summer echoes at very high latitudes
title_short Occurrence of polar mesosphere summer echoes at very high latitudes
title_full Occurrence of polar mesosphere summer echoes at very high latitudes
title_fullStr Occurrence of polar mesosphere summer echoes at very high latitudes
title_full_unstemmed Occurrence of polar mesosphere summer echoes at very high latitudes
title_sort occurrence of polar mesosphere summer echoes at very high latitudes
publisher Copernicus Publications
publishDate 2009
url https://doi.org/10.5194/angeo-27-1331-2009
https://doaj.org/article/fefe331304544d1b82463c6c8955f399
geographic Longyearbyen
Svalbard
geographic_facet Longyearbyen
Svalbard
genre Longyearbyen
Svalbard
genre_facet Longyearbyen
Svalbard
op_source Annales Geophysicae, Vol 27, Pp 1331-1342 (2009)
op_relation https://www.ann-geophys.net/27/1331/2009/angeo-27-1331-2009.pdf
https://doaj.org/toc/0992-7689
https://doaj.org/toc/1432-0576
doi:10.5194/angeo-27-1331-2009
0992-7689
1432-0576
https://doaj.org/article/fefe331304544d1b82463c6c8955f399
op_doi https://doi.org/10.5194/angeo-27-1331-2009
container_title Annales Geophysicae
container_volume 27
container_issue 3
container_start_page 1331
op_container_end_page 1342
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