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In the presence of the vertical temperature & wind-speed gradients, we extend Hines’ isothermal and shear-free model to calculate the vertical wavenumber (m r ) and growth rate (m i ) of gravity waves propagating in a stratified, non-isothermal, and wind-shear atmosphere. The profiles obtained from the extended Hines’ model are compared with those from the Wentzel-Kramers-Brillouin (WKB) approach up to 300 km altitude. The empirical neutral atmospheric and wind models (NRLMSISE-00 and HWM93) are used to obtain the vertical profiles of the meanfield properties and the zonal/meridional winds.
J. Z. G. Ma. 2016. \u201cEffects of Non Isothermality and Wind-Shears on the Propagation of Gravity Waves (I): Comparison between Hines Model and WKB Approach\u201d. Global Journal of Science Frontier Research - F: Mathematics & Decision GJSFR-F Volume 16 (GJSFR Volume 16 Issue F3): .
Crossref Journal DOI 10.17406/GJSFR
Print ISSN 0975-5896
e-ISSN 2249-4626
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Total Score: 131
Country: United States
Subject: Global Journal of Science Frontier Research - F: Mathematics & Decision
Authors: J. Z. G. Ma (PhD/Dr. count: 0)
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Publish Date: 2016 06, Tue
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In the presence of the vertical temperature & wind-speed gradients, we extend Hines’ isothermal and shear-free model to calculate the vertical wavenumber (m r ) and growth rate (m i ) of gravity waves propagating in a stratified, non-isothermal, and wind-shear atmosphere. The profiles obtained from the extended Hines’ model are compared with those from the Wentzel-Kramers-Brillouin (WKB) approach up to 300 km altitude. The empirical neutral atmospheric and wind models (NRLMSISE-00 and HWM93) are used to obtain the vertical profiles of the meanfield properties and the zonal/meridional winds.
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