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Ship tracks

  • Marine Cloud Brightening

    Marine Cloud Brightening

  • Studying Geoengineering with Natural and Anthropogenic Analogs

    Studying Geoengineering with Natural and Anthropogenic Analogs

  • Automated Underway Oceanic and Atmospheric Measurements from Ships

    Automated Underway Oceanic and Atmospheric Measurements from Ships

  • The Monterey Area Ship Track Experiment

    The Monterey Area Ship Track Experiment

  • Experimental Studies on Particle Emissions from Cruising Ship, Their Characteristic Properties, Transformation and Atmospheric Lifetime in the Marine Boundary Layer

    Experimental Studies on Particle Emissions from Cruising Ship, Their Characteristic Properties, Transformation and Atmospheric Lifetime in the Marine Boundary Layer

  • Observations of Ship Tracks from Ship-Based Platforms

    Observations of Ship Tracks from Ship-Based Platforms

  • Contrails, Contrail Cirrus, and Ship Tracks

    Contrails, Contrail Cirrus, and Ship Tracks

  • Marine Cloud Brightening

    Marine Cloud Brightening

  • Process-Modeling Study of Ship Tracks and Marine Cloud Brightening

    Process-Modeling Study of Ship Tracks and Marine Cloud Brightening

  • Real-Case Simulations of Aerosol–Cloud Interactions in Ship Tracks Over the Bay of Biscay

    Real-Case Simulations of Aerosol–Cloud Interactions in Ship Tracks Over the Bay of Biscay

  • Combustion Organic Aerosol As Cloud Condensation Nuclei in Ship Tracks Lynn M

    Combustion Organic Aerosol As Cloud Condensation Nuclei in Ship Tracks Lynn M

  • The Appearance and Disappearance of Ship Tracks on Large Spatial Scales

    The Appearance and Disappearance of Ship Tracks on Large Spatial Scales

  • How Well Do Large‐Eddy Simulations and Global Climate Models

    How Well Do Large‐Eddy Simulations and Global Climate Models

  • Switching Cloud Cover and Dynamical Regimes from Open to Closed Benard Cells in Response to the Suppression of Precipitation by Aerosols

    Switching Cloud Cover and Dynamical Regimes from Open to Closed Benard Cells in Response to the Suppression of Precipitation by Aerosols

  • Geoengineering: Parts I, Ii, and Iii

    Geoengineering: Parts I, Ii, and Iii

  • Comparing Ship-Track Droplet Sizes Inferred from Terra and Aqua MODIS Data

    Comparing Ship-Track Droplet Sizes Inferred from Terra and Aqua MODIS Data

  • “Solar” Geoengineering: What Is It? What Role Might It Play in an Overall Climate Strategy?

    “Solar” Geoengineering: What Is It? What Role Might It Play in an Overall Climate Strategy?

  • Weak Average Liquid-Cloud-Water Response to Anthropogenic Aerosols

    Weak Average Liquid-Cloud-Water Response to Anthropogenic Aerosols

Top View
  • Assessing the Potential Efficacy of Marine Cloud Brightening for Cooling Earth Using a Simple Heuristic Model
  • Ship-Track-Based Assessments Overestimate the Cooling Effect of Anthropogenic Aerosol Arxiv:2005.14159V1 [Physics.Ao-Ph] 28 Ma
  • Volcano and Ship Tracks Indicate Excessive Aerosol-Induced Cloud Water Increases in a Climate Model
  • Automatic Detection of Ship Tracks in ATSR-2 Satellite Imagery
  • Fossil Knowledge Shipping Forecast Is Partly Cloudy
  • Detecting Anthropogenic Cloud Perturbations with Deep Learning
  • Annual, Seasonal, and Interannual Variability of Air–Sea Heat Fluxes in the Indian Ocean
  • Aerosol Indirect Effects from Shipping Emissions: Sensitivity Studies with the Global Aerosol-Climate Model ECHAM-HAM
  • Modeling the Chemical Effects of Ship Exhaust in the Cloud-Free Marine Boundary Layer
  • Marine Cloud Brightening
  • Stratocumulus Clouds
  • Atmospheric Research 2019 Technical Highlights
  • 2. OBSERVATIONS During the FIRE Study of Marine Stratus Off the Coast of California in the Summer of 1987
  • Analysis of Ship Tracks in Cloudiness Transition Regions
  • ATMS 321 Human-‐Induced Global Warming Chapter 12
  • Emissions from Ships with Respect to Their Effects on Clouds
  • Cloud Condensation Nuclei and Ship Tracks
  • High Resolution (375 M) Cloud Microstructure As Seen from the NPP/VIIRS Satellite Imager D


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