Effects of Non Isothermality and Wind-Shears on the Propagation of Gravity Waves (I): Comparison between Hines Model and WKB Approach

Authors

  • J. Z. G. Ma

vertical temperature, wind-speed gradients, vertical wavenumber, Hines

Abstract

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.

How to Cite

Effects of Non Isothermality and Wind-Shears on the Propagation of Gravity Waves (I): Comparison between Hines Model and WKB Approach. (2016). Global Journal of Science Frontier Research, 16(17), 1-23. https://journalofscience.org/index.php/GJSFR/article/view/

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Effects of Non Isothermality and Wind-Shears on the Propagation of Gravity Waves (I): Comparison between Hines Model and WKB Approach

Published

2016-06-07

How to Cite

Effects of Non Isothermality and Wind-Shears on the Propagation of Gravity Waves (I): Comparison between Hines Model and WKB Approach. (2016). Global Journal of Science Frontier Research, 16(17), 1-23. https://journalofscience.org/index.php/GJSFR/article/view/