Three-Dimensional Turbulence-Resolving Modeling of the Venusian Cloud Layer and Induced Gravity Waves: Inclusion of Complete Radiative Transfer and Wind Shear
Author:
Affiliation:
1. Laboratoire de Météorologie Dynamique (IPSL), Sorbonne Université, Centre National de la Recherche Scientifique, École Polytechnique, École Normale Supérieure; Paris France
2. Institut Universitaire de France; Paris France
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018JE005679/fullpdf
Reference54 articles.
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3. Internal gravity waves generated by convective plumes;Ansong;Journal of Fluid Mechanics,2010
4. Mesoscale shallow convection in the atmosphere;Atkinson;Reviews of Geophysics,1996
5. Cloud-level penetrative compressible convection in the Venus atmosphere;Baker;Journal of the Atmospheric Sciences,1998
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