Review of Particle–Turbulence Interactions and Consequences for Cloud Physics

By P. Vaillancourt, M. Yau. 2000

182 citations recorded by the source corpus.

Subfields: Computational Mechanics, Earth-Surface Processes, Ocean Engineering

View Paper: https://www.semanticscholar.org/paper/ffef4944dd519e58addfad9f4c8d703652e771de

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In Computational Mechanics

In Earth-Surface Processes

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Citations in the corpus

Effects of in‐cloud nucleation and turbulence on droplet spectrum formation in cumulus clouds (2002, background): “It is worth noting in this connection that turbulence signi cantly in uences the rate of drop collisions, increasing the sweep-out volume (as well as frequency of collisions: Khain and Pinsky 1995, 1997 and Pinsky and Khain 1997; Zhou et al. 1998; Wang et al. 2000; Vaillancourt and Yau 2000) and t”
Growth of Cloud Droplets in a Turbulent Environment (2013, background): “Other relevant reviews, focusing on various aspects of cloud physics and the effects of cloud turbulence, are those by Beard & Ochs (1993), Jonas (1996), Vaillancourt & Yau (2000), and Khain et al. (2007).”
Microscopic approach to cloud droplet growth by condensation (2001, background): “…resolves the spatial and temporal evolution of such ambient conditions. a. Temporal and spatial scales associated with changes in ambient conditions of cloud droplets related to turbulence A discussion of the turbulent characteristics of cumulus clouds can be found in Vaillancourt and Yau (2000).”
PARTICLE-TURBULENCE INTERACTIONS IN ATMOSPHERIC CLOUDS (2003, background): “Finally, Vaillancourt & Yau (2000) have pointed out that the majority of numerical and laboratory work has been focused on a range of parameter space (e.g., Stokes number, gravitational sedimentation) different from that occupied by atmospheric clouds.”
Droplet growth in warm turbulent clouds (2012, background): “However, the extrapolation of these results to real clouds is not guaranteed: as pointed out by, for example, Grabowski and Vaillancourt (1999), Vaillancourt and Yau (2000), Wang et al. (2006a) and Khain et al. (2007), many DNS studies have been conducted without gravity, at moderate Reynolds…”
Turbulent clustering of stagnation points and inertial particles (2006, unknown): “Vaillancourt & Yau (2000) caution against droplet clustering mechanisms for explaining droplet spectral broadening in warm clouds because the Stokes numbers of cloud droplets are usually too small for them to be flung out of individual vortices and because the resulting concentration fluctuations m”
Observations of Small-Scale Turbulence and Energy Dissipation Rates in the Cloudy Boundary Layer (2006, background): “…air temperature in clouds using the ultrafast thermometers (UFT; Haman et al. 2001) are also on-hand and deliver data with centimeter resolution Vaillancourt and Yau (2000) pointed out that turbulence measurements with much higher resolution (than several meters) would be needed to investigate…”