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Raymond Shaw
Michigan Technological UniversityMeeting roles in:
Cloud Edge Entrainment Increases the Local Proportion of Large Droplets Through Slower Phase-Relaxation: Results from Airborne Holography and High Resolution LES
Evaluating Droplet Collision Theory in a Tall Convection-cloud Chamber Using Large-eddy Simulations with Lagrangian Microphysics
Lidar observations of vertically-resolved response of clouds to dry air entrainment
What have we learned about cloud microphysics from 10 years of Pi Chamber experiments and simulations? From supersaturation fluctuations, to haze-cloud interactions, to entrainment, to mixed-phase cloud equilibrium, to hygroscopic cloud seeding
Assessing the Role of Isobaric Mixing in Boundary-Layer Cloud Formation
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