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 se...

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Main Authors: M. Zecha, J. Röttger
Format: Article
Language:English
Published: Copernicus Publications 2009-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/27/1331/2009/angeo-27-1331-2009.pdf
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spelling doaj-fefe331304544d1b82463c6c8955f3992020-11-24T22:54:17ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762009-03-01271331134210.5194/angeo-27-1331-2009Occurrence of polar mesosphere summer echoes at very high latitudesM. Zecha0J. Röttger1Leibniz-Institut für Atmosphärenphysik, Kühlungsborn, GermanyEISCAT-CAWSES-Copernicus and Max-Planck Institute for Solar System Research, Katlenburg-Lindau, GermanyObservations 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.https://www.ann-geophys.net/27/1331/2009/angeo-27-1331-2009.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Zecha
J. Röttger
spellingShingle M. Zecha
J. Röttger
Occurrence of polar mesosphere summer echoes at very high latitudes
Annales Geophysicae
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
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2009-03-01
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.
url https://www.ann-geophys.net/27/1331/2009/angeo-27-1331-2009.pdf
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