Comparative studies of methods of obtaining AGW's propagation properties

Three among the existing methods of obtaining the properties (intrinsic period, wavelength, propagation direction) of atmospheric gravity waves (AGWs) were compared and studied by numerical method to simulate radar data. Three-dimensional fluctuation velocity satisfying dispersion equation and p...

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Main Authors: H. Y. Lue, F. S. Kuo
Format: Article
Language:English
Published: Copernicus Publications 2012-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/30/557/2012/angeo-30-557-2012.pdf
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spelling doaj-2d8a493e19b5472281e45e09937cec6b2020-11-25T00:18:54ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762012-03-013055757010.5194/angeo-30-557-2012Comparative studies of methods of obtaining AGW's propagation propertiesH. Y. Lue0F. S. Kuo1Department of Physics, Fu Jen University, Hsin Chuang, TaiwanDepartment of Electro-Optical Engineering, Vanung University, Chung-Li, TaiwanThree among the existing methods of obtaining the properties (intrinsic period, wavelength, propagation direction) of atmospheric gravity waves (AGWs) were compared and studied by numerical method to simulate radar data. Three-dimensional fluctuation velocity satisfying dispersion equation and polarization relation of atmospheric gravity wave were generated, then the numerical data were analysed by these methods to obtain the properties of waves. We found that, hodograph analysis was accurate for a monochromatic wave in obtaining its wave period and propagation direction, but the analysis became erratic for the case of multiple waves' superposition. The error was especially large when data consisted of both upward propagating waves and downward propagating waves. The hodograph method became meaningful again if all the component waves propagated in the same direction and the resulting period was dominantly decided by the lowest frequency wave. Stokes parameters method would obtain statistically meaningful values of wave period and azimuth if the spreading of the azimuths among the component waves did not exceed 90° and the resulting period and azimuth were dominated by the lowest frequency wave component as well, irrespective of the vertical sense of propagation. Another method called phase and group velocity tracing technique was reconfirmed to be meaningful in measuring the characteristic wave period and vertical group and phase velocities of a wave packet: the characteristic wave period and vertical wavelength was dominated by the wave with the highest frequency among the component waves in the wave packet. Based on these numerical results, a composite procedure of data analysis for wave propagation was proposed and an example of real data analysis was presented.https://www.ann-geophys.net/30/557/2012/angeo-30-557-2012.pdf
collection DOAJ
language English
format Article
sources DOAJ
author H. Y. Lue
F. S. Kuo
spellingShingle H. Y. Lue
F. S. Kuo
Comparative studies of methods of obtaining AGW's propagation properties
Annales Geophysicae
author_facet H. Y. Lue
F. S. Kuo
author_sort H. Y. Lue
title Comparative studies of methods of obtaining AGW's propagation properties
title_short Comparative studies of methods of obtaining AGW's propagation properties
title_full Comparative studies of methods of obtaining AGW's propagation properties
title_fullStr Comparative studies of methods of obtaining AGW's propagation properties
title_full_unstemmed Comparative studies of methods of obtaining AGW's propagation properties
title_sort comparative studies of methods of obtaining agw's propagation properties
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2012-03-01
description Three among the existing methods of obtaining the properties (intrinsic period, wavelength, propagation direction) of atmospheric gravity waves (AGWs) were compared and studied by numerical method to simulate radar data. Three-dimensional fluctuation velocity satisfying dispersion equation and polarization relation of atmospheric gravity wave were generated, then the numerical data were analysed by these methods to obtain the properties of waves. We found that, hodograph analysis was accurate for a monochromatic wave in obtaining its wave period and propagation direction, but the analysis became erratic for the case of multiple waves' superposition. The error was especially large when data consisted of both upward propagating waves and downward propagating waves. The hodograph method became meaningful again if all the component waves propagated in the same direction and the resulting period was dominantly decided by the lowest frequency wave. Stokes parameters method would obtain statistically meaningful values of wave period and azimuth if the spreading of the azimuths among the component waves did not exceed 90° and the resulting period and azimuth were dominated by the lowest frequency wave component as well, irrespective of the vertical sense of propagation. Another method called phase and group velocity tracing technique was reconfirmed to be meaningful in measuring the characteristic wave period and vertical group and phase velocities of a wave packet: the characteristic wave period and vertical wavelength was dominated by the wave with the highest frequency among the component waves in the wave packet. Based on these numerical results, a composite procedure of data analysis for wave propagation was proposed and an example of real data analysis was presented.
url https://www.ann-geophys.net/30/557/2012/angeo-30-557-2012.pdf
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