Microscopic approach to cloud droplet growth by condensation

By P. Vaillancourt. 2001

177 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Global and Planetary Change, Ocean Engineering

View Paper: https://www.semanticscholar.org/paper/a750dce22fd6e52bd3c130f374c53b1fd108739f

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In Earth-Surface Processes

In Global and Planetary Change

In Ocean Engineering

Citations in the corpus

Growth of Cloud Droplets in a Turbulent Environment (2013, methodology): “First, they neglected the latent heating term (i.e., the last term on the right-hand side of Equation 1), which can lead to unrealistically large supersaturation fluctuations, as documented by Vaillancourt et al. (2002), Lanotte et al. (2009), and Sidin et al. (2009).”
Confronting the Challenge of Modeling Cloud and Precipitation Microphysics (2020, background): “Accelerated drop growth and SD broadening can also occur from drop clustering (e.g., Shaw, 2000; Vaillancourt et al., 2002) and turbulent impacts on collision‐coalescence of similar size drops (Chandrakar, Cantrell, Kostinski, et al., 2018; Chandrakar, Cantrell, & Shaw, 2018; Chen, Yau, &…”
Analyzing preferential concentration and clustering of inertial particles in turbulence (2012, background): “Squires and Eaton (1990, 1991), Wang and Maxey (1993), Vaillancourt et al. (2002), and Tanaka et al. (2002) show simultaneous visualizations of vorticity and particle concentration isocontours obtained from spatial slices of direct numerical simulations that clearly show a strong correlation…”
PARTICLE-TURBULENCE INTERACTIONS IN ATMOSPHERIC CLOUDS (2003, methodology): “…of the distribution of particles resulting from a direct numerical simulation of homogeneous, isotropic turbulence containing cloud droplets (with realistic Stokes number and energy dissipation rate; see Vaillancourt et al. 2002) is shown in Figure 6, to be discussed in greater detail in Section 5.”
Droplet growth in warm turbulent clouds (2012, methodology): “Vaillancourt et al. (2002) were the first to study the condensational growth of droplets in 3-”
Homogeneous and Inhomogeneous Mixing in Cumulus Clouds: Dependence on Local Turbulence Structure (2009, background): “Droplet sedimentation may also influence the microphysical response to mixing because it allows droplets to move across fluid streamlines (e.g., Jensen and Baker 1989; Vaillancourt et al. 2002).”