All Stories

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