A case study of a sporadic sodium layer observed by the ALOMAR Weber Na LIDAR

1071 1081 Several possible mechanisms for the production of sporadic sodium layers have been discussed in the literature, but none of them seem to explain all the accumulated observations. The hypotheses range from direct meteoric input, to energetic electron bombardment on meteoric smoke particles,...

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Published in:Annales Geophysicae
Main Authors: Nesse, H., Heinrich, D., Williams, B., Hoppe, U.-P., Stadsnes, J., Rietveld, M., Singer, W., Blum, Ulrich, Sandanger, M.I., Trondsen, E.
Format: Article in Journal/Newspaper
Language:English
Published: 2008
Subjects:
Online Access:https://publica.fraunhofer.de/handle/publica/215814
https://doi.org/10.5194/angeo-26-1071-2008
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author Nesse, H.
Heinrich, D.
Williams, B.
Hoppe, U.-P.
Stadsnes, J.
Rietveld, M.
Singer, W.
Blum, Ulrich
Sandanger, M.I.
Trondsen, E.
author_facet Nesse, H.
Heinrich, D.
Williams, B.
Hoppe, U.-P.
Stadsnes, J.
Rietveld, M.
Singer, W.
Blum, Ulrich
Sandanger, M.I.
Trondsen, E.
author_sort Nesse, H.
collection Publikationsdatenbank der Fraunhofer-Gesellschaft
container_issue 5
container_start_page 1071
container_title Annales Geophysicae
container_volume 26
description 1071 1081 Several possible mechanisms for the production of sporadic sodium layers have been discussed in the literature, but none of them seem to explain all the accumulated observations. The hypotheses range from direct meteoric input, to energetic electron bombardment on meteoric smoke particles, to ion neutralization, to temperature dependent chemistry. The varied instrumentation located on Andoya and near Tromso in Norway gives us an opportunity to test the different theories applied to high latitude sporadic sodium layers. We use the ALOMAR Weber sodium lidar to monitor the appearance and characteristics of a sporadic sodium layer that was observed on 5 November 2005. We also monitor the temperature to test the hypotheses regarding a temperature dependent mechanism. The EISCAT Tromso Dynasonde, the ALOMAR/UiO All-sky camera and the SKiYMET meteor radar on Andoya are used to test the suggested relationships of sporadic sodium layers and sporadic E-layers, electron precipitation, and meteor deposition during this event. We find that more than one candidate is eligible to explain our observation of the sporadic sodium layer. 26 5
format Article in Journal/Newspaper
genre EISCAT
Tromso
Tromso
genre_facet EISCAT
Tromso
Tromso
geographic Alomar
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geographic_facet Alomar
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op_doi https://doi.org/10.5194/angeo-26-1071-2008
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spelling ftfrauneprints:oai:publica.fraunhofer.de:publica/215814 2025-04-06T14:51:14+00:00 A case study of a sporadic sodium layer observed by the ALOMAR Weber Na LIDAR Nesse, H. Heinrich, D. Williams, B. Hoppe, U.-P. Stadsnes, J. Rietveld, M. Singer, W. Blum, Ulrich Sandanger, M.I. Trondsen, E. 2008 https://publica.fraunhofer.de/handle/publica/215814 https://doi.org/10.5194/angeo-26-1071-2008 en eng Annales Geophysicae https://publica.fraunhofer.de/handle/publica/215814 atmospheric composition and structure ion chemistry of the atmosphere thermosphere-composition and chemistry ionosphere ionosphere-atmosphere interactions ionospheric irregularity 620 551 journal article 2008 ftfrauneprints https://doi.org/10.5194/angeo-26-1071-2008 2025-03-10T08:42:55Z 1071 1081 Several possible mechanisms for the production of sporadic sodium layers have been discussed in the literature, but none of them seem to explain all the accumulated observations. The hypotheses range from direct meteoric input, to energetic electron bombardment on meteoric smoke particles, to ion neutralization, to temperature dependent chemistry. The varied instrumentation located on Andoya and near Tromso in Norway gives us an opportunity to test the different theories applied to high latitude sporadic sodium layers. We use the ALOMAR Weber sodium lidar to monitor the appearance and characteristics of a sporadic sodium layer that was observed on 5 November 2005. We also monitor the temperature to test the hypotheses regarding a temperature dependent mechanism. The EISCAT Tromso Dynasonde, the ALOMAR/UiO All-sky camera and the SKiYMET meteor radar on Andoya are used to test the suggested relationships of sporadic sodium layers and sporadic E-layers, electron precipitation, and meteor deposition during this event. We find that more than one candidate is eligible to explain our observation of the sporadic sodium layer. 26 5 Article in Journal/Newspaper EISCAT Tromso Tromso Publikationsdatenbank der Fraunhofer-Gesellschaft Alomar ENVELOPE(-67.083,-67.083,-68.133,-68.133) Norway Tromso ENVELOPE(16.546,16.546,68.801,68.801) Annales Geophysicae 26 5 1071 1081
spellingShingle atmospheric composition and structure
ion chemistry of the atmosphere
thermosphere-composition and chemistry
ionosphere
ionosphere-atmosphere interactions
ionospheric irregularity
620
551
Nesse, H.
Heinrich, D.
Williams, B.
Hoppe, U.-P.
Stadsnes, J.
Rietveld, M.
Singer, W.
Blum, Ulrich
Sandanger, M.I.
Trondsen, E.
A case study of a sporadic sodium layer observed by the ALOMAR Weber Na LIDAR
title A case study of a sporadic sodium layer observed by the ALOMAR Weber Na LIDAR
title_full A case study of a sporadic sodium layer observed by the ALOMAR Weber Na LIDAR
title_fullStr A case study of a sporadic sodium layer observed by the ALOMAR Weber Na LIDAR
title_full_unstemmed A case study of a sporadic sodium layer observed by the ALOMAR Weber Na LIDAR
title_short A case study of a sporadic sodium layer observed by the ALOMAR Weber Na LIDAR
title_sort case study of a sporadic sodium layer observed by the alomar weber na lidar
topic atmospheric composition and structure
ion chemistry of the atmosphere
thermosphere-composition and chemistry
ionosphere
ionosphere-atmosphere interactions
ionospheric irregularity
620
551
topic_facet atmospheric composition and structure
ion chemistry of the atmosphere
thermosphere-composition and chemistry
ionosphere
ionosphere-atmosphere interactions
ionospheric irregularity
620
551
url https://publica.fraunhofer.de/handle/publica/215814
https://doi.org/10.5194/angeo-26-1071-2008