Collision efficiency of droplets across diffusive, electrostatic and inertial regimes
Florian Poydenot, Bruno Andreotti

TL;DR
This paper reviews and quantitatively investigates the collision mechanisms of droplets in clouds across diffusive, electrostatic, and inertial regimes, revealing a size gap where collision rates are minimized due to competing effects.
Contribution
It provides a comprehensive analysis of droplet collision mechanisms across regimes and identifies a size range with low collision probability, using an open-source Monte Carlo simulation.
Findings
Inertia dominates for large drops with Stokes number > 1.
Thermal diffusion dominates for small drops with Péclet number < 1.
A size gap (1-10 μm) exists where collision rates are minimized due to competing effects.
Abstract
Rain drops form in clouds by collision of submillimetric droplets falling under gravity: larger drops fall faster than smaller ones and collect them on their path. The puzzling stability of fogs and non-precipitating warm clouds with respect to this avalanching mechanism has been a longstanding problem. How to explain that droplets of diameter around have a low probability of collision, inhibiting the cascade towards larger and larger drops? Here we review the dynamical mechanisms that have been proposed in the literature and quantitatively investigate the frequency of drop collisions induced by Brownian diffusion, electrostatics and gravity, using an open-source Monte-Carlo code that takes all of them into account. Inertia dominates over aerodynamic forces for large drops, when the Stokes number is larger than . Thermal diffusion dominates over aerodynamic forces…
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Taxonomy
TopicsParticle Dynamics in Fluid Flows · Electrohydrodynamics and Fluid Dynamics · Fluid Dynamics and Heat Transfer
