All Stories

  1. Are turbulence effects on droplet collision–coalescence a key to understanding observed rain formation in clouds?
  2. Lagrangian and Eulerian Supersaturation Statistics in Turbulent Cloudy Rayleigh–Bénard Convection: Applications for LES Subgrid Modeling
  3. Evolution of Droplet Size Distributions During the Transition of an Ultraclean Stratocumulus Cloud System to Open Cell Structure: An LES Investigation Using Lagrangian Microphysics
  4. Comparison of Lagrangian Superdroplet and Eulerian Double-Moment Spectral Microphysics Schemes in Large-Eddy Simulations of an Isolated Cumulus Congestus Cloud
  5. Supersaturation Variability from Scalar Mixing: Evaluation of a New Subgrid-Scale Model Using Direct Numerical Simulations of Turbulent Rayleigh–Bénard Convection
  6. Observed and Bin Model Simulated Evolution of Drop Size Distributions in High‐Based Cumulus Congestus Over the United Arab Emirates
  7. Influences of Environmental Relative Humidity and Horizontal Scale of Subcloud Ascent on Deep Convective Initiation
  8. Impact of entrainment-mixing and turbulent fluctuations on droplet size distributions in a cumulus cloud: An investigation using Lagrangian microphysics with a sub-grid-scale model
  9. Supersaturation fluctuations in moist turbulent Rayleigh–Bénard convection: a two-scalar transport problem
  10. Droplet size distributions in turbulent clouds: experimental evaluation of theoretical distributions
  11. Extensive Soot Compaction by Cloud Processing from Laboratory and Field Observations
  12. Aerosol‐Mediated Glaciation of Mixed‐Phase Clouds: Steady‐State Laboratory Measurements
  13. Dispersion Aerosol Indirect Effect in Turbulent Clouds: Laboratory Measurements of Effective Radius
  14. Influence of Turbulent Fluctuations on Cloud Droplet Size Dispersion and Aerosol Indirect Effects
  15. Observation of a link between energy dissipation rate and oscillation frequency of the large-scale circulation in dry and moist Rayleigh-Bénard turbulence
  16. Influence of Microphysical Variability on Stochastic Condensation in a Turbulent Laboratory Cloud
  17. TURBULENCE-INDUCED CLOUD CLEANSING
  18. A Laboratory Facility to Study Gas–Aerosol–Cloud Interactions in a Turbulent Environment: The Π Chamber
  19. Aerosol indirect effect from turbulence-induced broadening of cloud-droplet size distributions