001     35907
005     20240712100853.0
024 7 _ |a 10.1029/2004JD004752
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024 7 _ |a WOS:000224876600011
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024 7 _ |a 0141-8637
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024 7 _ |a 2128/20574
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037 _ _ |a PreJuSER-35907
041 _ _ |a eng
082 _ _ |a 550
084 _ _ |2 WoS
|a Meteorology & Atmospheric Sciences
100 1 _ |a Ern, M.
|b 0
|u FZJ
|0 P:(DE-Juel1)VDB13497
245 _ _ |a Absolute values of gravity wave momentum flux derived from satellite data
260 _ _ |c 2004
|a Washington, DC
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300 _ _ |a D20103
336 7 _ |a Journal Article
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336 7 _ |a article
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440 _ 0 |a Journal of Geophysical Research D: Atmospheres
|x 0148-0227
|0 6393
|v 109
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a [1] Temperature data obtained by the Cryogenic Infrared Spectrometers and Telescopes for the Atmosphere (CRISTA) are analyzed for gravity waves (GWs). Amplitude, phase and vertical wavelength are determined from detrended temperature height profiles. The retrieved phases are utilized to estimate the horizontal wavelengths. At 25 km altitude an equatorial maximum of horizontal wavelength with a decrease toward mid and high latitudes is found. Simultaneous estimates of both horizontal and vertical wavelengths and temperature amplitudes allow the direct calculation of GW momentum flux (MF) from satellite observations for the first time. However, histograms of horizontal wavelength distributions indicate severe undersampling which prevents the retrieval of the propagation directions of the waves, and suggests our MF estimates may be too low, particularly at the high latitudes. Therefore an empirical aliasing correction has been applied. A world map of MF at 25 km altitude shows high variability and pronounced source regions and deviates in structure from a map of GW variances at the same altitude. Results from the Warner and McIntyre GW parameterization scheme (three-part model) show better agreement with CRISTA MF estimates than with CRISTA squared GW amplitudes. Best agreement is found for low model launch levels. Large error ranges of the estimated MF values obtained in this paper could be substantially reduced by improved horizontal sampling in future satellite missions.
536 _ _ |a Chemie und Dynamik der Geo-Biosphäre
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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 satellite remote sensing
700 1 _ |a Preusse, P.
|b 1
|u FZJ
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700 1 _ |a Alexander, M. J.
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700 1 _ |a Warner, C. D.
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773 _ _ |0 PERI:(DE-600)2016800-7
|a 10.1029/2004JD004752
|g Vol. 109, p. D20103
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|q 109|t Journal of Geophysical Research
|v 109
|x 0148-0227
|y 2004
|t Journal of geophysical research / Atmospheres
856 7 _ |u http://dx.doi.org/10.1029/2004JD004752
856 4 _ |u https://juser.fz-juelich.de/record/35907/files/2004JD004752.pdf
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913 1 _ |k U01
|v Chemie und Dynamik der Geo-Biosphäre
|l Chemie und Dynamik der Geo-Biosphäre
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914 1 _ |y 2004
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