On the role of an anisotropic gravity wave spectrum in maintaining the circulation of the middle atmosphere
- 15 February 1998
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 25 (4) , 509-512
- https://doi.org/10.1029/98gl50177
Abstract
No abstract availableKeywords
This publication has 13 references indexed in Scilit:
- Radiative‐dynamical climatology of the first‐generation Canadian middle atmosphere modelAtmosphere-Ocean, 1997
- Empirical model of 90–120 km horizontal winds from wind‐imaging interferometer green line measurements in 1992–1993Journal of Geophysical Research: Atmospheres, 1997
- Doppler-spread parameterization of gravity-wave momentum deposition in the middle atmosphere. Part 1: Basic formulationJournal of Atmospheric and Solar-Terrestrial Physics, 1997
- Middle Atmosphere Simulations with the ECHAM4 Model: Sensitivity to the Doppler Spread Gravity Wave ParameterizationPublished by Springer Nature ,1997
- Seasonal Simulations with the Canadian Middle Atmosphere Model: Sensitivity to a combination of orographic and Doppler Spread Parameterizations of Gravity Wave DragPublished by Springer Nature ,1997
- The Role of Parameterized Drag in a Troposphere-Stratosphere-Mesosphere General Circulation ModelPublished by Springer Nature ,1997
- The Parameterization of Gravity Wave Drag Based on the Nonlinear Diffusion of Wave SpectraPublished by Springer Nature ,1997
- Sponge layer feedbacks in middle‐atmosphere modelsJournal of Geophysical Research: Atmospheres, 1996
- Vertical evolution of gravity wave spectra and the parameterization of associated wave dragJournal of Geophysical Research: Atmospheres, 1995
- Long-period motions in the equatorial mesosphereJournal of Atmospheric and Terrestrial Physics, 1993