All Stories

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