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  5. Investigation of gravity wave activity based on NDMC, NDACC and CTBTO measurements
 
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Investigation of gravity wave activity based on NDMC, NDACC and CTBTO measurements

Author(s)
Wüst, S.  
Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen (DLR), Germany  
Schmidt, C.  
Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen (DLR), Germany  
Kramer, R.  
Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen (DLR), Germany  
Bittner, M.  
Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen (DLR), Germany  
Hauchecorne, A.  
Centre national de la recherche scientifique (CNRS), France  
Keckhut, P.  
Centre national de la recherche scientifique (CNRS), France  
LePichon, A.  
Commissariat à l’énergie atomique et aux énergies alternatives (CEA), France  
Marchetti, E.  
Università degli studi di firenze (UNIFI)  
Mze, N.  
Centre national de la recherche scientifique (CNRS), France  
Pecora, E.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Type
Abstract
Language
English
Obiettivo Specifico
2A. Fisica dell'alta atmosfera
Status
Published
Journal
European Geosciences Union General Assembly  
Date Issued
April 27, 2014
Conference Location
Vienna, Austria
URI
https://www.earth-prints.org/handle/2122/9988
Subjects

gravity wave activity...

Abstract
GRIPS (Ground based Infrared P-branch Spectrometer) airglow measurements allow the derivation of kinetic temperature in the mesopause region during night with a temporal resolution of 10s to 15s. Amongst others, these time series can be used for the investigation of atmospheric dynamics like gravity wave activity. GRIPS measurements are performed in the framework of NDMC – the international Network for the Detection of Mesospheric Change. The project ARISE combines NDMC, NDACC (Network for the Detection of Atmospheric Composition Change) and CTBTO (Comprehensive Nuclear-Test-Ban Treaty Organization)measurements to infer a new 3D image of atmospheric dynamics from ground to mesopause. In this context, GRIPS data of about two to three years collected at the Observatory Haute-Provence, France and Catania, Italy are utilized to derive an index for shortand long-period gravity wave activity on daily and seasonal base. This time period includes also a stratospheric warming event. Potential energy density is calculated and compared with NDACC measurements at Haute-Provence; differences are discussed. For the measurements at the Italian station, comparisons of gravity wave and volcanic activity relying on infrasound array and seismic measurements are performed. First hints for volcanic induced mesopause gravity wave activity are presented.
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EGU2014-11747-1.pdf

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Abstract
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Checksum (MD5)

14c48641c258637ce677dbc08d79840f

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