001     57885
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024 7 _ |2 DOI
|a 10.1016/j.jastp.2007.07.005
024 7 _ |2 WOS
|a WOS:000251841800009
037 _ _ |a PreJuSER-57885
041 _ _ |a eng
082 _ _ |a 530
084 _ _ |2 WoS
|a Geochemistry & Geophysics
084 _ _ |2 WoS
|a Meteorology & Atmospheric Sciences
100 1 _ |a Fröhlich, K.
|b 0
|0 P:(DE-HGF)0
245 _ _ |a The global distribution of gravity wave energy in the lower stratosphere derived from GPS data and gravity wave modelling: Attempt and challenges
260 _ _ |a Amsterdam [u.a.]
|b Elsevier Science
|c 2007
300 _ _ |a 2238 - 2248
336 7 _ |a Journal Article
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336 7 _ |a Journal Article
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336 7 _ |a ARTICLE
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336 7 _ |a JOURNAL_ARTICLE
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336 7 _ |a article
|2 DRIVER
440 _ 0 |a Journal of Atmospheric and Solar-Terrestrial Physics
|x 1364-6826
|0 14744
|v 69
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Five years of global temperatures retrieved from radio occultations measured by Champ (Challenging Minisatellite Payload) and SAC-C (Satelite de Aplicaciones Cientificas-C) are analyzed for gravity waves (GWs). In order to separate GWs from other atmospheric variations, a high-pass filter was applied on the vertical profile. Resulting temperature fluctuations correspond to vertical wavelengths between 400 in (instrumental resolution) and 10 km (limit of the high-pass filter). The temperature fluctuations can be converted into GW potential energy, but for comparison with parameterization schemes GW momentum flux is required. We therefore used representative values for the vertical and horizontal wavelength to infer GW momentum flux from the GPS measurements. The vertical wavelength value is determined by high-pass filtering, the horizontal wavelength is adopted from a latitude-dependent climatology. The obtained momentum flux distributions agree well, both in global distribution and in absolute values, with simulations using the Warner and McIntyre parameterization (WM) scheme. However, discrepancies are found in the annual cycle. Online simulations, implementing the WM scheme in the mechanistic COMMA-LIM (Cologne Model of the Middle Atmosphere-Leipzig Institute for Meteorology) general circulation model (GCM), do not converge, demonstrating that a good representation of GWs in a GCM requires both a realistic launch distribution and an adequate representation of GW breaking and momentum transfer. (c) 2007 Elsevier Ltd. All rights reserved.
536 _ _ |a Atmosphäre und Klima
|c P22
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588 _ _ |a Dataset connected to Web of Science
650 _ 7 |a J
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653 2 0 |2 Author
|a gravity waves
653 2 0 |2 Author
|a momentum flux
653 2 0 |2 Author
|a parameterization scheme
653 2 0 |2 Author
|a GPS
700 1 _ |a Schmidt, T.
|b 1
|0 P:(DE-HGF)0
700 1 _ |a Ern, M.
|b 2
|u FZJ
|0 P:(DE-Juel1)VDB13497
700 1 _ |a Preusse, P.
|b 3
|u FZJ
|0 P:(DE-Juel1)VDB12001
700 1 _ |a de la Torre, A.
|b 4
|0 P:(DE-HGF)0
700 1 _ |a Wickert, J.
|b 5
|0 P:(DE-HGF)0
700 1 _ |a Jacobi, Ch.
|b 6
|0 P:(DE-HGF)0
773 _ _ |a 10.1016/j.jastp.2007.07.005
|g Vol. 69, p. 2238 - 2248
|p 2238 - 2248
|q 69<2238 - 2248
|0 PERI:(DE-600)2020910-1
|t Journal of atmospheric and solar-terrestrial physics
|v 69
|y 2007
|x 1364-6826
856 7 _ |u http://dx.doi.org/10.1016/j.jastp.2007.07.005
909 C O |o oai:juser.fz-juelich.de:57885
|p VDB
913 1 _ |k P22
|v Atmosphäre und Klima
|l Atmosphäre und Klima
|b Umwelt
|z fortgesetzt als P23
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|x 0
914 1 _ |y 2007
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
920 1 _ |k ICG-1
|l Stratosphäre
|d 30.09.2010
|g ICG
|0 I:(DE-Juel1)VDB790
|x 1
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980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)ICE-4-20101013
981 _ _ |a I:(DE-Juel1)IEK-7-20101013


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