All Stories

  1. Aerosol–cloud interactions in marine low-clouds in a warmer climate
  2. A Model Intercomparison Study to Investigate Mixing Characteristics in Non‐Precipitating Stratocumulus Clouds
  3. Capturing and explaining the effects of three-dimensional radiative transfer on cloud evolution with the dynamic TenStream solver
  4. Exploiting Ergodocity, Space-Time Exchange, and the Deborah number in Aerosol-Cloud Interaction Studies
  5. Secondary Ice Production Invigorates Updrafts but Suppresses Precipitation in Simulated Subtropical Convection
  6. The optimal size distribution of seeding aerosol for marine cloud brightening: insights from emulating a Lagrangian cloud model
  7. A Robust Aerosol Impact on Clouds Along the Subtropical to Tropical Transition
  8. Supplementary material to "A Robust Aerosol Impact on Clouds Along the Subtropical to Tropical Transition"
  9. Aging of Droplet Size Distribution in Stratocumulus Clouds: Regimes of Droplet Size Distribution Evolution
  10. Impacts of Environmental Conditions and Ice Nuclei Recycling on Arctic Mixed-Phase Cloud Properties
  11. Quasi-Lagrangian observations of cloud transitions during the initial phase of marine cold air outbreaks in the Arctic – Part 2: Vertical cloud structure
  12. The Chemical Mechanism Integrator Cminor v1.0: a stand-alone Fortran environment for the particle-based simulation of chemical multiphase mechanisms
  13. Marine Cloud Brightening of Cumulus Clouds: From the Sprayer to the Cloud
  14. Opinion: Inferring process from snapshots of cloud systems
  15. On the processes determining the slope of cloud water adjustments in weakly and non-precipitating stratocumulus
  16. Aerosol-Cloud Interactions in Marine Low-Clouds in a Warmer Climate
  17. Magnitude and timescale of liquid water path adjustments to cloud droplet number concentration perturbations for nocturnal non-precipitating marine stratocumulus
  18. Does small-scale turbulence matter for ice growth in mixed-phase clouds?
  19. The critical number and size of precipitation embryos to accelerate warm rain initiation
  20. Opinion: Inferring Process from Snapshots of Cloud Systems
  21. Supplementary material to "The Chemical Mechanism Integrator Cminor v1.0: A Stand-Alone Fortran Environment for the Particle-Based Simulation of Chemical Multiphase Mechanisms"
  22. The Chemical Mechanism Integrator Cminor v1.0: A Stand-Alone Fortran Environment for the Particle-Based Simulation of Chemical Multiphase Mechanisms
  23. Dissecting cirrus clouds: navigating effects of turbulence on homogeneous ice formation
  24. Microphysics regimes due to haze–cloud interactions: cloud oscillation and cloud collapse
  25. Clouds' Clout on the Aerosol Size Distribution - Modelling Detailed Chemical Processing
  26. Impacts of Entrainment and Mixing on Ice Growth in Mixed-Phase Clouds
  27. Regimes of Droplet Size Distribution Evolution in Stratocumulus: From Adiabatic Growth to Entrainment and Mixing
  28. Does small-scale turbulence matter for ice growth in mixed-phase clouds?
  29. On the Processes Determining the Slope of Cloud-Water Adjustments in Non-Precipitating Stratocumulus
  30. Magnitude and timescale of liquid water path adjustments to cloud droplet number concentration perturbations for nocturnal non-precipitating marine stratocumulus
  31. On the Processes Determining the Slope of Cloud-Water Adjustments in Non-Precipitating Stratocumulus
  32. Supplementary material to "Magnitude and timescale of liquid water path adjustments to cloud droplet number concentration perturbations for nocturnal non-precipitating marine stratocumulus"
  33. The impact of aerosol on cloud water: a heuristic perspective
  34. Diurnal evolution of non-precipitating marine stratocumuli in a large-eddy simulation ensemble
  35. The Critical Number and Size of Precipitation Embryos to Accelerate Warm Rain Initiation
  36. Supplementary material to "The Impact of Aerosol on Cloud Water: A Heuristic Perspective"
  37. The Impact of Aerosol on Cloud Water: A Heuristic Perspective
  38. Microphysics regimes due to haze-cloud interactions: cloud oscillation and cloud collapse
  39. Life Cycle Evolution of Mixing in Shallow Cumulus Clouds
  40. Diurnal evolution of non-precipitating marine stratocumuli in an LES ensemble
  41. Supplementary material to "Diurnal evolution of non-precipitating marine stratocumuli in an LES ensemble"
  42. Physical science research needed to evaluate the viability and risks of marine cloud brightening
  43. Sensitivities of Marine Cloud Brightening Studied with a Lagrangian Cloud Model
  44. Marine-cloud brightening: an airborne concept
  45. Effects of intermittent aerosol forcing on the stratocumulus-to-cumulus transition
  46. Life Cycle Evolution of Inhomogeneous Mixing in Shallow Cumulus Clouds
  47. On the Roles of Precipitation and Entrainment in Stratocumulus Transitions between Mesoscale States
  48. The Effects of Aerosol on Small‐Scale Cloud‐Environment Mixing: Implications for Simulating and Observing Inhomogeneous Mixing
  49. Effects of Intermittent Aerosol Forcing on the Stratocumulus-to-Cumulus Transition
  50. Paths from Aerosol Particles to Activation and Cloud Droplets in Shallow Cumulus Clouds: The Roles of Entrainment and Supersaturation Fluctuations
  51. A Note on Aerosol Processing by Droplet Collision‐Coalescence
  52. Evaluation of Pulse Aerosol Forcing on Marine Stratocumulus Clouds in the Context of Marine Cloud Brightening
  53. Toward a Numerical Benchmark for Warm Rain Processes
  54. An Intercomparison of Large‐Eddy Simulations of a Convection Cloud Chamber Using Haze‐Capable Bin and Lagrangian Cloud Microphysics Schemes
  55. Between Broadening and Narrowing: How Mixing Affects the Width of the Droplet Size Distribution
  56. The Small-Scale Mixing of Clouds with their Environment: Impacts on Micro-and Macroscale Cloud Properties
  57. Paths from Aerosol Particles to Activation and Cloud Droplets in Shallow Cumulus Clouds: The Roles of Entrainment and Supersaturation Fluctuation
  58. A Parameterization of Interstitial Aerosol Extinction and Its Application to Marine Cloud Brightening
  59. Observing short-timescale cloud development to constrain aerosol–cloud interactions
  60. Gaussian-process emulation for integrating data-driven aerosol-cloud physics from simulation, satellite, and ground-based data
  61. The Present and Future of Lagrangian Cloud Modeling: From the Centimeter to Kilometer Scale
  62. Observing short timescale cloud development to constrain aerosol-cloud interactions
  63. Exploring the Influence of the Duration of Aerosol Perturbations on Cloud Responses
  64. Cloud Microphysical Implications for Marine Cloud Brightening: The Importance of the Seeded Particle Size Distribution
  65. Aerosol-cloud-climate cooling overestimated by ship-track data
  66. Collisional growth in a particle-based cloud microphysical model: insights from column model simulations using LCM1D (v1.0)
  67. Liquid Water Path Steady States in Stratocumulus: Insights from Process-Level Emulation and Mixed-Layer Theory
  68. Effects of Entrainment and Mixing on the Wegener-Bergeron-Findeisen Process
  69. Collection/Aggregation in a Lagrangian cloud microphysical model: Insights from column model applications
  70. Overview of the PALM model system 6.0
  71. Beyond Cloud Microphysics: Representing Subgrid-Scale Processes in Lagrangian Cloud Models
  72. Collection/Aggregation in a Lagrangian cloud microphysical model: Insights from column model applications using LCM1D (v0.9)
  73. Anthropogenic Air Pollution Delays Marine Stratocumulus Break‐up to Open‐Cells
  74. An emulator approach to stratocumulus susceptibility
  75. Toward Large‐Eddy Simulations of Dust Devils of Observed Intensity: Effects of Grid Spacing, Background Wind, and Surface Heterogeneities
  76. Can liquid cloud microphysical processes be used for vertically pointing cloud radar calibration?
  77. Entrainment and Mixing in Stratocumulus: Effects of a New Explicit Subgrid-Scale Scheme for Large-Eddy Simulations with Particle-Based Microphysics
  78. Can liquid cloud microphysical processes be used for vertically-pointing cloud radar calibration?
  79. An emulator approach to stratocumulus susceptibility
  80. Inhomogeneous Mixing in Lagrangian Cloud Models: Effects on the Production of Precipitation Embryos
  81. A Cloud Microphysics Parameterization for Shallow Cumulus Clouds Based on Lagrangian Cloud Model Simulations
  82. Improving collisional growth in Lagrangian cloud models: development and verification of a new splitting algorithm
  83. Improving Collisional Growth in Lagrangian Cloud Models: Development and Verification of a New Splitting Algorithm
  84. On the limits of Köhler activation theory: how do collision and coalescence affect the activation of aerosols?
  85. The Route to Raindrop Formation in a Shallow Cumulus Cloud Simulated by a Lagrangian Cloud Model
  86. On the Limits of Köhler Activation Theory: How do Collision and Coalescence Affect the Activation of Aerosols?
  87. On the Limits of Köhler Activation Theory: How do Collision and Coalescence Affect the Activation of Aerosols?
  88. Collection/aggregation algorithms in Lagrangian cloud microphysical models: rigorous evaluation in box model simulations
  89. On the Limits of Köhler Activation Theory: How do Collision and Coalescence Affect the Activation of Aerosols?
  90. Collection/aggregation algorithms in Lagrangian cloud microphysical models: Rigorous evaluation in box model simulations
  91. Large-Eddy Simulations of Dust Devils and Convective Vortices
  92. The Effect of Spurious Cloud Edge Supersaturations in Lagrangian Cloud Models: An Analytical and Numerical Study
  93. The Parallelized Large-Eddy Simulation Model (PALM) version 4.0 for atmospheric and oceanic flows: model formulation, recent developments, and future perspectives
  94. Entrainment of aerosols and their activation in a shallow cumulus cloud studied with a coupled LCM–LES approach
  95. The Parallelized Large-Eddy Simulation Model (PALM) version 4.0 for atmospheric and oceanic flows: model formulation, recent developments, and future perspectives
  96. Entrainment and mixing at the interface of shallow cumulus clouds: Results from a combination of observations and simulations