Equatorward Propagation of Inertia–Gravity Waves due to Steady and Intermittent Wave Sources
- 1 June 2003
- journal article
- Published by American Meteorological Society in Journal of the Atmospheric Sciences
- Vol. 60 (11), 1410-1419
- https://doi.org/10.1175/1520-0469(2003)060<1410:epoiwd>2.0.co;2
Abstract
A simple ray-tracing model for the equatorward propagation of inertia–gravity waves in the lower stratosphere is investigated. The model is based on a zonally symmetric wave source and incorporates radiative wave damping. It is shown that steady extratropical wave sources are able to produce spectra of potential energy that exhibit a conspicuous peak at the equator, which resembles the spectral peaks that are often observed in field data. This reinforces the recent suggestion by other authors that such peaks are caused by the latitudinal variation of the local Coriolis parameter, though these authors did not consider horizontal wave propagation. Notably, horizontal wave propagation can produce equatorial peaks even with strictly extratropical wave sources. Wave source intermittency is then investigated by allowing for a time-dependent wave source. The source is treated statistically as a stationary random process and a number of general comments are made with respect to the impact of intermittenc... Abstract A simple ray-tracing model for the equatorward propagation of inertia–gravity waves in the lower stratosphere is investigated. The model is based on a zonally symmetric wave source and incorporates radiative wave damping. It is shown that steady extratropical wave sources are able to produce spectra of potential energy that exhibit a conspicuous peak at the equator, which resembles the spectral peaks that are often observed in field data. This reinforces the recent suggestion by other authors that such peaks are caused by the latitudinal variation of the local Coriolis parameter, though these authors did not consider horizontal wave propagation. Notably, horizontal wave propagation can produce equatorial peaks even with strictly extratropical wave sources. Wave source intermittency is then investigated by allowing for a time-dependent wave source. The source is treated statistically as a stationary random process and a number of general comments are made with respect to the impact of intermittenc...Keywords
This publication has 9 references indexed in Scilit:
- Latitudinal Variations Observed in Gravity Waves with Short Vertical WavelengthsJournal of the Atmospheric Sciences, 2002
- Experimental probability density functions of small-scale fluctuations in the stably stratified atmosphereJournal of Fluid Mechanics, 2000
- A Spectral Parameterization of Mean-Flow Forcing due to Breaking Gravity WavesJournal of the Atmospheric Sciences, 1999
- On Shear-Generated Gravity Waves that Reach the Mesosphere. Part II: Wave PropagationJournal of the Atmospheric Sciences, 1999
- On Shear-Generated Gravity Waves that Reach the Mesosphere. Part I: Wave GenerationJournal of the Atmospheric Sciences, 1999
- Body force circulations in a compressible atmosphere: Key conceptsPure and Applied Geophysics, 1989
- The Radiative Damping of Short Vertical Scale Waves in the MesosphereJournal of the Atmospheric Sciences, 1984
- The Influence of Gravity Wave Breaking on the General Circulation of the Middle AtmosphereJournal of the Atmospheric Sciences, 1983
- A Parameterization of Scale-Dependent Radiative Damping Rates in the Middle AtmosphereJournal of the Atmospheric Sciences, 1982