The focus of this paper is on the numerical solution of the stochastic collection equation–stochastic breakup equation (SCE–SBE) describing the evolution of raindrop spectra in warm rain. The drop size distribution (DSD) is discretized using the fixed-pivot scheme proposed by Kumar and Ramkrishna, and new discrete equations for solving collision breakup are presented. The model is evaluated using established coalescence and breakup parameterizations (kernels) available in the literature, and in that regard this paper provides a substantial review of the relevant science. The challenges posed by the need to achieve stable and accurate numerical solutions of the SCE–SBE are examined in detail. In particular, this paper focuses on the impact o...
International audienceModels of coalescence and breakup lead to equilibrium of the raindrop size dis...
Warm rain collision coalescence has been persistently difficult to parameterize in the bulk microphy...
In the last stage of droplet growth in clouds which leads to drizzle formation, larger droplets begi...
A study of the evolution of raindrop spectra (raindrop size distribution, DSD) between cloud base an...
Numerous laboratory and numerical studies have been dedicated to understanding collisional breakup a...
The study of the vertical evolution of raindrop size distributions (DSDs) during rainfall, from the ...
Includes bibliographical references (leaves 121-126)A computational study is made of the variation o...
Warm rain collision-coalescence has been persistently difficult to parameterize in bulk microphysics...
Both numerical modeling and laboratory experiments document the possibility of a raindrop size distr...
Numerical investigations of binary raindrop collisions, comprising the drop pairs of Low and List (1...
The data contained herein are the post-processed disdrometer observational data and numerical simula...
An open question in warm rain process and precipitation formation is how rain forms in warm cumulus ...
Stochasticity of the collisional growth of cloud droplets is studied using the super-droplet method...
A microscopic model of warm clouds involving input of water droplets, dropletdroplet aggregation, dr...
An open question in cloud physics is how rain forms in warm cumulus as rapidly as it is sometimes ob...
International audienceModels of coalescence and breakup lead to equilibrium of the raindrop size dis...
Warm rain collision coalescence has been persistently difficult to parameterize in the bulk microphy...
In the last stage of droplet growth in clouds which leads to drizzle formation, larger droplets begi...
A study of the evolution of raindrop spectra (raindrop size distribution, DSD) between cloud base an...
Numerous laboratory and numerical studies have been dedicated to understanding collisional breakup a...
The study of the vertical evolution of raindrop size distributions (DSDs) during rainfall, from the ...
Includes bibliographical references (leaves 121-126)A computational study is made of the variation o...
Warm rain collision-coalescence has been persistently difficult to parameterize in bulk microphysics...
Both numerical modeling and laboratory experiments document the possibility of a raindrop size distr...
Numerical investigations of binary raindrop collisions, comprising the drop pairs of Low and List (1...
The data contained herein are the post-processed disdrometer observational data and numerical simula...
An open question in warm rain process and precipitation formation is how rain forms in warm cumulus ...
Stochasticity of the collisional growth of cloud droplets is studied using the super-droplet method...
A microscopic model of warm clouds involving input of water droplets, dropletdroplet aggregation, dr...
An open question in cloud physics is how rain forms in warm cumulus as rapidly as it is sometimes ob...
International audienceModels of coalescence and breakup lead to equilibrium of the raindrop size dis...
Warm rain collision coalescence has been persistently difficult to parameterize in the bulk microphy...
In the last stage of droplet growth in clouds which leads to drizzle formation, larger droplets begi...