Effect of turbulence on collisional growth of cloud droplets
arXiv:1711.10062 · doi:10.1175/JAS-D-18-0081.1
Abstract
We investigate the effect of turbulence on the collisional growth of um-sized droplets through high- resolution numerical simulations with well resolved Kolmogorov scales, assuming a collision and coalescence efficiency of unity. The droplet dynamics and collisions are approximated using a superparticle approach. In the absence of gravity, we show that the time evolution of the shape of the droplet-size distribution due to turbulence-induced collisions depends strongly on the turbulent energy-dissipation rate, but only weakly on the Reynolds number. This can be explained through the energy dissipation rate dependence of the mean collision rate described by the Saffman-Turner collision model. Consistent with the Saffman-Turner collision model and its extensions, the collision rate increases as the square root of the energy dissipation rate even when coalescence is invoked. The size distribution exhibits power law behavior with a slope of -3.7 between a maximum at approximately 10 um up to about 40 um. When gravity is invoked, turbulence is found to dominate the time evolution of an initially monodisperse droplet distribution at early times. At later times, however, gravity takes over and dominates the collisional growth. We find that the formation of large droplets is very sensitive to the turbulent energy dissipation rate. This is due to the fact that turbulence enhances the collisional growth between similar sized droplets at the early stage of raindrop formation. The mean collision rate grows exponentially, which is consistent with the theoretical prediction of the continuous collisional growth even when turbulence-generated collisions are invoked. This consistency only reflects the mean effect of turbulence on collisional growth.
References in corpus (11)
- Caustic activation of rain showers
- Sling effect in collisions of water droplets in turbulent clouds
- A representative particle approach to coagulation and fragmentation of dust aggregates and fluid droplets
- Simple Viscous Flows: from Boundary Layers to the Renormalization Group
- Eulerian and modified Lagrangian approaches to multi-dimensional condensation and collection
- Colliding Particles in Highly Turbulent Flows
- A Condensation-Coalescence Cloud Model for Exoplanetary Atmospheres: Formulation and Test Applications to Terrestrial and Jovian Clouds
- Advective collisions
- Variable-range Projection Model for Turbulence-driven Collisions
- Relative velocities in bidisperse turbulent suspensions
- Collisions of particles advected in random flows
Cited by in corpus (6)
- Large-eddy simulations of marine boundary-layer clouds associated with cold air outbreaks during the ACTIVATE campaign-part 1: Case setup and sensitivities to large-scale forcings
- Condensational and collisional growth of cloud droplets in a turbulent environment
- Potential quantum advantage for simulation of fluid dynamics
- Cloud-droplet growth due to supersaturation fluctuations in stratiform clouds
- Collision fluctuations of lucky droplets with superdroplets
- Coagulation of inertial particles in supersonic turbulence