Simultaneous observations of a Mesospheric Inversion Layer and turbulence during the ECOMA-2010 rocket campaign

From 19 November to 19 December 2010 the fourth and final ECOMA rocket campaign was conducted at Andøya Rocket Range (69 N, 16 E) in northern Norway. We present and discuss measurement results obtained during the last rocket launch labelled ECOMA09 when simultaneous and true common volume in situ me...

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Main Authors: Szewczyk, A., Strelnikov, B., Rapp, M., Strelnikova, I., Baumgarten, G., Kaifler, N., Dunker, T., Hoppe, U.-P.
Format: Article in Journal/Newspaper
Language:English
Published: Göttingen : Copernicus 2013
Subjects:
550
Online Access:https://oa.tib.eu/renate/handle/123456789/5613
https://doi.org/10.34657/4242
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spelling ftleibnizopen:oai:oai.leibnizopen.de:3lu88IgBdbrxVwz6D6fb 2023-07-16T03:51:44+02:00 Simultaneous observations of a Mesospheric Inversion Layer and turbulence during the ECOMA-2010 rocket campaign Szewczyk, A. Strelnikov, B. Rapp, M. Strelnikova, I. Baumgarten, G. Kaifler, N. Dunker, T. Hoppe, U.-P. 2013 application/pdf https://oa.tib.eu/renate/handle/123456789/5613 https://doi.org/10.34657/4242 eng eng Göttingen : Copernicus CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ Annales Geophysicae 31 (2013), 5 Meteorology and atmospheric dynamics (Middle atmosphere dynamics Turbulence Waves and tides) atmospheric dynamics atmospheric tide atmospheric wave inversion layer mesosphere Andoya Norway Vesteralen 550 article Text 2013 ftleibnizopen https://doi.org/10.34657/4242 2023-06-25T23:38:38Z From 19 November to 19 December 2010 the fourth and final ECOMA rocket campaign was conducted at Andøya Rocket Range (69 N, 16 E) in northern Norway. We present and discuss measurement results obtained during the last rocket launch labelled ECOMA09 when simultaneous and true common volume in situ measurements of temperature and turbulence supported by ground-based lidar observations reveal two Mesospheric Inversion Layers (MIL) at heights between 71 and 73 km and between 86 and 89 km. Strong turbulence was measured in the region of the upper inversion layer, with the turbulent energy dissipation rates maximising at 2 W kg-1. This upper MIL was observed by the ALOMAR Weber Na lidar over the period of several hours. The spatial extension of this MIL as observed by the MLS instrument onboard AURA satellite was found to be more than two thousand kilometres. Our analysis suggests that both observed MILs could possibly have been produced by neutral air turbulence. publishedVersion Article in Journal/Newspaper Andøya Northern Norway LeibnizOpen (The Leibniz Association) Alomar ENVELOPE(-67.083,-67.083,-68.133,-68.133) Andøya ENVELOPE(13.982,13.982,68.185,68.185) Norway
institution Open Polar
collection LeibnizOpen (The Leibniz Association)
op_collection_id ftleibnizopen
language English
topic Meteorology and atmospheric dynamics (Middle atmosphere dynamics
Turbulence
Waves and tides)
atmospheric dynamics
atmospheric tide
atmospheric wave
inversion layer
mesosphere
Andoya
Norway
Vesteralen
550
spellingShingle Meteorology and atmospheric dynamics (Middle atmosphere dynamics
Turbulence
Waves and tides)
atmospheric dynamics
atmospheric tide
atmospheric wave
inversion layer
mesosphere
Andoya
Norway
Vesteralen
550
Szewczyk, A.
Strelnikov, B.
Rapp, M.
Strelnikova, I.
Baumgarten, G.
Kaifler, N.
Dunker, T.
Hoppe, U.-P.
Simultaneous observations of a Mesospheric Inversion Layer and turbulence during the ECOMA-2010 rocket campaign
topic_facet Meteorology and atmospheric dynamics (Middle atmosphere dynamics
Turbulence
Waves and tides)
atmospheric dynamics
atmospheric tide
atmospheric wave
inversion layer
mesosphere
Andoya
Norway
Vesteralen
550
description From 19 November to 19 December 2010 the fourth and final ECOMA rocket campaign was conducted at Andøya Rocket Range (69 N, 16 E) in northern Norway. We present and discuss measurement results obtained during the last rocket launch labelled ECOMA09 when simultaneous and true common volume in situ measurements of temperature and turbulence supported by ground-based lidar observations reveal two Mesospheric Inversion Layers (MIL) at heights between 71 and 73 km and between 86 and 89 km. Strong turbulence was measured in the region of the upper inversion layer, with the turbulent energy dissipation rates maximising at 2 W kg-1. This upper MIL was observed by the ALOMAR Weber Na lidar over the period of several hours. The spatial extension of this MIL as observed by the MLS instrument onboard AURA satellite was found to be more than two thousand kilometres. Our analysis suggests that both observed MILs could possibly have been produced by neutral air turbulence. publishedVersion
format Article in Journal/Newspaper
author Szewczyk, A.
Strelnikov, B.
Rapp, M.
Strelnikova, I.
Baumgarten, G.
Kaifler, N.
Dunker, T.
Hoppe, U.-P.
author_facet Szewczyk, A.
Strelnikov, B.
Rapp, M.
Strelnikova, I.
Baumgarten, G.
Kaifler, N.
Dunker, T.
Hoppe, U.-P.
author_sort Szewczyk, A.
title Simultaneous observations of a Mesospheric Inversion Layer and turbulence during the ECOMA-2010 rocket campaign
title_short Simultaneous observations of a Mesospheric Inversion Layer and turbulence during the ECOMA-2010 rocket campaign
title_full Simultaneous observations of a Mesospheric Inversion Layer and turbulence during the ECOMA-2010 rocket campaign
title_fullStr Simultaneous observations of a Mesospheric Inversion Layer and turbulence during the ECOMA-2010 rocket campaign
title_full_unstemmed Simultaneous observations of a Mesospheric Inversion Layer and turbulence during the ECOMA-2010 rocket campaign
title_sort simultaneous observations of a mesospheric inversion layer and turbulence during the ecoma-2010 rocket campaign
publisher Göttingen : Copernicus
publishDate 2013
url https://oa.tib.eu/renate/handle/123456789/5613
https://doi.org/10.34657/4242
long_lat ENVELOPE(-67.083,-67.083,-68.133,-68.133)
ENVELOPE(13.982,13.982,68.185,68.185)
geographic Alomar
Andøya
Norway
geographic_facet Alomar
Andøya
Norway
genre Andøya
Northern Norway
genre_facet Andøya
Northern Norway
op_source Annales Geophysicae 31 (2013), 5
op_rights CC BY 3.0 Unported
https://creativecommons.org/licenses/by/3.0/
op_doi https://doi.org/10.34657/4242
_version_ 1771542231324295168