Entrainment, Mixing, and Microphysics in Trade-Wind Cumulus
By H. Gerber, Glendon Frick, Jorgen B. Jensen, J. Hudson. 2008
176 citations recorded by the source corpus.
Subfields: Atmospheric Science, Earth-Surface Processes, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/6e4a48000651730de39f84084d788fc26084100b
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- J. Brenguier
- Lance R. Collins
- John Christos Vassilicos
- Wojciech W. Grabowski
- P. Bartello
- Chidong Zhang
- David A. Randall
- Hugh Morrison
In Earth-Surface Processes
- Wojciech W. Grabowski
- Lian-Ping Wang
- Lance R. Collins
- J. Brenguier
- M. Reeks
- R. Ijzermans
- Szymon P. Malinowski
- John Christos Vassilicos
In Global and Planetary Change
- Lian-Ping Wang
- Wojciech W. Grabowski
- J. Brenguier
- Lance R. Collins
- John Christos Vassilicos
- P. Bartello
- Chidong Zhang
- David A. Randall
Citations in the corpus
- Large‐eddy simulation of the transient and near‐equilibrium behavior of precipitating shallow convection (2015, unknown): “, 2006; Gerber et al., 2008]. In a comprehensive study of the microphysical conditions during RICO, Hudson and Noble [2014] find a mean cloud droplet number density of 89 cm(23) with a standard deviation of 30 cm(23).”
- Droplet growth in warm turbulent clouds (2012, background): “…incloud activation leads to approximately constant-in-height mean cloud droplet concentration in shallow cumuli, in agreement with aircraft observations (e.g. Gerber et al., 2008; Arabas et al., 2009) but in contrast to simulations where activation above the cloud base is artificially suppressed.”