171 p.Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 1997.Despite the time and space constraints placed on the results by the observed evolution of the updrafts, the calculations showed that the process of rain formation in warm convective clouds is simple and efficient, provided that giant and ultragiant CCN are present near cloud base. While more complex processes leading to drop spectra broadening, such as mixing, and stochastic condensation most likely also occur in nature, they appear to be unnecessary to explain the rapid formation of rain in warm convective clouds.U of I OnlyRestricted to the U of I community idenfinitely during batch ingest of legacy ETD
In-situ measurements in convective clouds (up to the freezing level) over the Amazon basin show that...
We present a mean-field model of cloud evolution that describes droplet growth due to condensation a...
We present a mean-field model of cloud evolution that describes droplet growth due to condensation a...
171 p.Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 1997.Despite the time and space co...
Deep convective clouds play a key role in tropical weather patterns, summertime rainfall, and the gl...
Space-borne observations reveal that 20–40% of marine convective clouds below the freezing level pro...
In-situ measurements in convective clouds (up to the freezing level) over the Amazon basin show that...
Space-borne observations reveal that 20–40% of marine convective clouds below the freezing level pro...
Space-borne observations reveal that 20–40% of marine convective clouds below the freezing level pro...
A parametrization of the rain formation in warm clouds is developed which includes the effects of tu...
A parametrization of the rain formation in warm clouds is developed which includes the effects of tu...
A parametrization of the rain formation in warm clouds is developed which includes the effects of tu...
In-situ measurements in convective clouds (up to the freezing level) over the Amazon basin show that...
Two simple heuristic model formulations for warm rain formation are introduced and their behavior ex...
International audienceIn-situ measurements in convective clouds (up to the freezing level) over the ...
In-situ measurements in convective clouds (up to the freezing level) over the Amazon basin show that...
We present a mean-field model of cloud evolution that describes droplet growth due to condensation a...
We present a mean-field model of cloud evolution that describes droplet growth due to condensation a...
171 p.Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 1997.Despite the time and space co...
Deep convective clouds play a key role in tropical weather patterns, summertime rainfall, and the gl...
Space-borne observations reveal that 20–40% of marine convective clouds below the freezing level pro...
In-situ measurements in convective clouds (up to the freezing level) over the Amazon basin show that...
Space-borne observations reveal that 20–40% of marine convective clouds below the freezing level pro...
Space-borne observations reveal that 20–40% of marine convective clouds below the freezing level pro...
A parametrization of the rain formation in warm clouds is developed which includes the effects of tu...
A parametrization of the rain formation in warm clouds is developed which includes the effects of tu...
A parametrization of the rain formation in warm clouds is developed which includes the effects of tu...
In-situ measurements in convective clouds (up to the freezing level) over the Amazon basin show that...
Two simple heuristic model formulations for warm rain formation are introduced and their behavior ex...
International audienceIn-situ measurements in convective clouds (up to the freezing level) over the ...
In-situ measurements in convective clouds (up to the freezing level) over the Amazon basin show that...
We present a mean-field model of cloud evolution that describes droplet growth due to condensation a...
We present a mean-field model of cloud evolution that describes droplet growth due to condensation a...