Gravity wave breaking, secondary wave generation, and mixing above deep convection in a three‐dimensional cloud model
- 15 December 2006
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 33 (23)
- https://doi.org/10.1029/2006gl027988
Abstract
No abstract availableKeywords
This publication has 18 references indexed in Scilit:
- Some Effects of Model Resolution on Simulated Gravity Waves Generated by Deep, Mesoscale ConvectionJournal of the Atmospheric Sciences, 2005
- Mixing Layer Formation near the Tropopause Due to Gravity Wave–Critical Level Interactions in a Cloud-Resolving ModelJournal of the Atmospheric Sciences, 2004
- A cloud model interpretation of jumping cirrus above storm topGeophysical Research Letters, 2004
- Breaking of thunderstorm‐generated gravity waves as a source of short‐period ducted waves at mesopause altitudesGeophysical Research Letters, 2003
- An Investigation of Turbulence Generation Mechanisms above Deep ConvectionJournal of the Atmospheric Sciences, 2003
- Moisture plumes above thunderstorm anvils and their contributions to cross‐tropopause transport of water vapor in midlatitudesJournal of Geophysical Research: Solid Earth, 2003
- Gravity waves generated by the dry convective boundary layer: Two‐dimensional scale selection and boundary‐layer feedbackQuarterly Journal of the Royal Meteorological Society, 2002
- Gravity waves generated by the dry convective boundary layer: Two-dimensional scale selection and boundary-layer feedbackQuarterly Journal of the Royal Meteorological Society, 2002
- Gravity waves in the mesosphere generated by tropospheric conventionTellus A: Dynamic Meteorology and Oceanography, 1999
- Turbulent mixing by breaking gravity wavesJournal of Fluid Mechanics, 1998