Persistent layers of enhanced C2N in the lower stratosphere from VHF radar observations
- 1 January 2001
- journal article
- Published by American Geophysical Union (AGU) in Radio Science
- Vol. 36 (1), 137-149
- https://doi.org/10.1029/2000rs002318
Abstract
No abstract availableKeywords
This publication has 33 references indexed in Scilit:
- Inertia-gravity waves in the troposphere and lower stratosphere associated with a jet stream exit regionAnnales Geophysicae, 1999
- Long-period unstable gravity-waves and associated VHF radar echoesAnnales Geophysicae, 1997
- Zenith-angle dependence of VHF specular reflection echoes in the lower atmosphereJournal of Atmospheric and Solar-Terrestrial Physics, 1997
- Energy dissipation rates, eddy diffusivity, and the Prandtl number: An in situ experimental approach and its consequences on radar estimate of turbulent parametersRadio Science, 1997
- Gravity waves in the stratosphere and troposphere observed by lidar and MST radarJournal of Atmospheric and Terrestrial Physics, 1994
- A statistical study of the structure, saturation and sources of inertio-gravity waves in the lower stratosphere observed with the MU radarJournal of Atmospheric and Terrestrial Physics, 1994
- The Coupling of Gravity Waves and Turbulence at White Sands, New Mexico, from VHF Radar ObservationsJournal of Applied Meteorology and Climatology, 1993
- Fine Altitude Resolution Observations of Stratospheric Turbulent Layers by the Arecibo 430 MHz RadarJournal of the Atmospheric Sciences, 1982
- Use of Doppler radar for the measurement of atmospheric turbulence parameters from the intensity of clear‐air echoesRadio Science, 1980
- Tropopause Detection by Partial Specular Reflection with Very-High-Frequency RadarScience, 1979