All Stories

  1. Impacts of Bulk Microphysics Scheme Structural Choices on Simulations of Rain Initiation Through Drop Coalescence
  2. Counteracting influences of gravitational settling modulate aerosol impacts on cloud-base-lowering fog characteristics
  3. Counteracting Influences of Gravitational Settling Modulate Aerosol Impacts on Cloud Base Lowering Fog Characteristics
  4. Processes Controlling the Entrainment and Liquid Water Response to Aerosol Perturbations in Nonprecipitating Stratocumulus Clouds
  5. Bulk Microphysics Schemes May Perform Better With a Unified Cloud‐Rain Category
  6. Above-cloud concentrations of cloud condensation nuclei help to sustain some Arctic low-level clouds
  7. Opinion: A critical evaluation of the evidence for aerosol invigoration of deep convection
  8. Identifying Important Microphysical Properties and Processes for Marine Fog Forecasts
  9. Dissipation of Mixed-Phase Arctic Clouds and Its Relationship to Aerosol Properties - Final Technical Report
  10. Above Cloud CCN Concentrations Help to Sustain Some Arctic Low-Level Clouds
  11. Opinion: A Critical Evaluation of the Evidence for Aerosol Invigoration of Deep Convection
  12. A Bin and a Bulk Microphysics Scheme Can Be More Alike Than Two Bin Schemes
  13. Do Arctic mixed-phase clouds sometimes dissipate due to insufficient aerosol? Evidence from comparisons between observations and idealized simulations
  14. Limitations of Separate Cloud and Rain Categories in Parameterizing Collision‐Coalescence for Bulk Microphysics Schemes
  15. Arctic Mixed-Phase Clouds Sometimes Dissipate Due to Insufficient Aerosol - Evidence from Idealized Large Eddy Simulations
  16. What drives increased evaporation at cloud top in polluted stratocumulus clouds?
  17. Limitations of separate cloud and rain categories in parameterizing collision-coalescence for bulk microphysics schemes
  18. Arctic mixed-phase clouds sometimes dissipate due to insufficient aerosol: evidence from observations and idealized simulations
  19. Demistify: a large-eddy simulation (LES) and single-column model (SCM) intercomparison of radiation fog
  20. Cloud Top Radiative Cooling Rate Drives Non‐Precipitating Stratiform Cloud Responses to Aerosol Concentration
  21. Recognition of Inter‐Cloud Versus Intra‐Cloud Controls on Droplet Dispersion With Applications to Microphysics Parameterization
  22. Invigoration or Enervation of Convective Clouds by Aerosols?
  23. Processes contributing to cloud dissipation and formation events on the North Slope of Alaska
  24. The importance of Aitken mode aerosol particles for cloud sustenance in the summertime high Arctic – a simulation study supported by observational data
  25. Processes contributing to Arctic cloud dissipation and formation events that bookend clear sky periods
  26. The importance of Aitken mode aerosol particles for cloud sustenance in the summertime high Arctic: A simulation study supported by observational data
  27. Environmental Controls on Tropical Sea Breeze Convection and Resulting Aerosol Redistribution
  28. Using an Arbitrary Moment Predictor to Investigate the Optimal Choice of Prognostic Moments in Bulk Cloud Microphysics Schemes
  29. Relative sensitivities of simulated rainfall to fixed shape parameters and collection efficiencies
  30. Meteorological and Land Surface Properties Impacting Sea Breeze Extent and Aerosol Distribution in a Dry Environment
  31. The free troposphere as a potential source of arctic boundary layer aerosol particles
  32. The role of the gamma function shape parameter in determining differences between condensation rates in bin and bulk microphysics schemes
  33. The Importance of the Shape of Cloud Droplet Size Distributions in Shallow Cumulus Clouds. Part I: Bin Microphysics Simulations
  34. The Importance of the Shape of Cloud Droplet Size Distributions in Shallow Cumulus Clouds. Part II: Bulk Microphysics Simulations
  35. Reply to RC1
  36. Reply to RC2
  37. Reply to SC1
  38. The Role of the Size Distribution Shape in Determining Differences between Condensation Rates in Bin and Bulk Microphysics Schemes
  39. Make It a Double? Sobering Results from Simulations Using Single-Moment Microphysics Schemes
  40. Sensitivity of Warm-Frontal Processes to Cloud-Nucleating Aerosol Concentrations
  41. The role of latent heating in warm frontogenesis
  42. Fluorescent visualization of a spreading surfactant