Cause of a monochromatic inertia‐gravity wave breaking observed by the MU radar
Open Access
- 1 November 1988
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 15 (12) , 1349-1352
- https://doi.org/10.1029/gl015i012p01349
Abstract
No abstract availableKeywords
This publication has 9 references indexed in Scilit:
- Formation of mesospheric VHF echoing layers due to a gravity wave motionJournal of Atmospheric and Terrestrial Physics, 1988
- VHF radar measurements of small-scale and meso-scale dynamical processes in the middle atmospherePhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1987
- Characteristics of mesospheric internal gravity waves observed by MU RadarGeophysical Research Letters, 1987
- Convective and dynamical instabilities due to gravity wave motions in the lower and middle atmosphere: Theory and observationsRadio Science, 1985
- The Role of Gravity Wave Induced Drag and Diffusion in the Momentum Budget of the MesosphereJournal of the Atmospheric Sciences, 1982
- A Quasi One-Dimensional Model of the Middle Atmosphere Circulation Interacting with Internal Gravity WavesJournal of the Meteorological Society of Japan. Ser. II, 1982
- Turbulence and stress owing to gravity wave and tidal breakdownJournal of Geophysical Research: Oceans, 1981
- Formation of the thermocline step structure by large-amplitude internal gravity wavesJournal of Geophysical Research, 1969
- Generation of turbulence in the upper atmosphere by internal gravity wavesJournal of Geophysical Research, 1967