The role of gravity wave generated advection and diffusion in transport of tracers in the mesosphere
- 20 September 1988
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 93 (D9), 11075-11082
- https://doi.org/10.1029/jd093id09p11075
Abstract
No abstract availableKeywords
This publication has 24 references indexed in Scilit:
- A Model of Stationary Gravity Wave Breakdown with Convective AdjustmentJournal of the Atmospheric Sciences, 1988
- Mean winds of the upper middle atmosphere (∼70–110 km) from the global radar network: Comparisons with CIRA 72, and new rocket and satellite dataAdvances in Space Research, 1987
- The effect of breaking gravity waves on the dynamics and chemical composition of the mesosphere and lower thermosphereJournal of Geophysical Research: Atmospheres, 1985
- Fluxes of Heat and Constituents Due to Convectively Unstable Gravity WavesJournal of the Atmospheric Sciences, 1985
- The vertical distribution of ozone in the mesosphere and lower thermosphereJournal of Geophysical Research: Atmospheres, 1984
- On the Linear Approximation of Gravity Wave Saturation in the MesosphereJournal of the Atmospheric Sciences, 1984
- An Accurate Radiative Heating and Cooling Algorithm for Use in a Dynamical Model of the Middle AtmosphereJournal of the Atmospheric Sciences, 1982
- A numerical model of the zonal mean circulation of the middle atmospherePure and Applied Geophysics, 1980
- On the Mean Meridional Mass Motions of the Stratosphere and MesosphereJournal of the Atmospheric Sciences, 1978
- Generation of turbulence in the upper atmosphere by internal gravity wavesJournal of Geophysical Research, 1967