All Stories

  1. Development of the Horizontal Cloud Condensation Nuclei Counter (HCCNC) to detect particle activation down to 4 °C temperature and 0.05 % supersaturation
  2. Supplementary material to "The State of Diversity, Equity, and Inclusion in the Cloud Physics Community"
  3. The State of Diversity, Equity, and Inclusion in the Cloud Physics Community
  4. Aviation soot is unlikely to impact natural cirrus clouds
  5. Microfluidic Immersion Freezing of Binary Mineral Mixtures Containing Microcline, Montmorillonite, or Quartz
  6. Ice Nucleating Particle Concentrations over the Eurasian-Arctic seas
  7. Quantified ice-nucleating ability of AgI-containing seeding particles in natural clouds
  8. Development of a Horizontal Cloud Condensation Nuclei Counter (HCCNC) to detect particle activation at temperatures below 4 °C and supersaturations below 0.05 %
  9. Correction to “Surface Formation Pathway of Nitrogen- and Sulfur-Containing Organic Compounds on Ammonium Sulfate”
  10. Comparing ice-nucleating particles in extensive stratiform clouds
  11. Surface Formation Pathway of Nitrogen- and Sulfur-Containing Organic Compounds on Ammonium Sulfate
  12. Advancing understanding on aviation's non-CO2 climate effects through combination of numerical modelling and observations: ACACIA
  13. Perspectives on the Desert dust Contribution to Ice Nucleation in Mixed-phase Clouds and Associated Radiative Forcing
  14. Ice nucleation onto model nanoplastics in the cirrus cloud regime
  15. Terrestrial and marine sources of ice nucleating particles in the Eurasian Arctic
  16. Links between atmospheric aerosols and sea state in the Arctic Ocean
  17. Quantified ice-nucleating ability of AgI-containing seeding particles in natural clouds
  18. Formation of Sodium Chloride on the Surface of Sulfate-Rich Gobi Desert Salt in Response to Water Adsorption
  19. Simulated contrail-processed aviation soot aerosols are poor ice-nucleating particles at cirrus temperatures
  20. Glucose Enhances Salinity-Driven Sea Spray Aerosol Production in Eastern Arctic Waters
  21. Soot aerosols from commercial aviation engines are poor ice-nucleating particles at cirrus cloud temperatures
  22. Critical Size of Silver Iodide Containing Glaciogenic Cloud Seeding Particles
  23. Influence of Lowering Soot‐Water Contact Angle on Ice Nucleation of Ozone‐Aged Soot
  24. Critical Size of Silver Iodide Containing Glaciogenic Cloud Seeding Particles
  25. Two new multirotor uncrewed aerial vehicles (UAVs) for glaciogenic cloud seeding and aerosol measurements within the CLOUDLAB project
  26. Contrail processed aviation soot aerosol are poor ice nucleating particles at cirrus temperatures
  27. Soot aerosol from commercial aviation engines are poor ice nucleating particles at cirrus cloud temperatures
  28. Development and characterization of the Portable Ice Nucleation Chamber 2 (PINCii)
  29. Two new multirotor UAVs for glaciogenic cloud seeding and aerosol measurements within the CLOUDLAB project
  30. Adsorbed Water Promotes Chemically Active Environments on the Surface of Sodium Chloride
  31. Overview of ambient ice nucleation measurements from 1949 – 2
  32. The importance of soot-water contact angle in soot ice nucleation ability in the cirrus regime
  33. The state of diversity, equity and inclusion in the cloud physics community
  34. Understanding the Abundance, Variability and Sources of Ice NucleatingParticles (INPs) over the Kara and Laptev Seas in the Eurasian Arctic
  35. Development and characterization of the Portable Ice Nucleation Chamber 2 (PINCii)
  36. Unexpected Behavior of Chloride and Sulfate Ions upon Surface Solvation of Martian Salt Analogue
  37. Physicochemical properties of charcoal aerosols derived from biomass pyrolysis affect their ice-nucleating abilities at cirrus and mixed-phase cloud conditions
  38. Impacts of Cloud‐Processing on Ice Nucleation of Soot Particles Internally Mixed With Sulfate and Organics
  39. Potential impacts of atmospheric microplastics and nanoplastics on cloud formation processes
  40. Predicting atmospheric background number concentration of ice-nucleating particles in the Arctic
  41. The Ny-Ålesund Aerosol Cloud Experiment (NASCENT): Overview and First Results
  42. The Microfluidic Ice Nuclei Counter Zürich (MINCZ): a platform for homogeneous and heterogeneous ice nucleation
  43. Impacts of Simulated Contrail Processing and Organic Content Change on the Ice Nucleation of Soot Particles
  44. Physicochemical properties affect ice nucleating abilities of biomass burning derived charcoal aerosols at cirrus and mixed-phase cloud conditions
  45. Retrieving ice-nucleating particle concentration and ice multiplication factors using active remote sensing validated by in situ observations
  46. The diurnal and seasonal variability of ice-nucleating particles at the High Altitude Station Jungfraujoch (3580 m a.s.l.), Switzerland
  47. Ice-nucleating particles from multiple aerosol sources in the urban environment of Beijing under mixed-phase cloud conditions
  48. The Microfluidic Ice Nuclei Counter Zürich (MINCZ): A platform for homogeneous and heterogeneous ice nucleation
  49. Laboratory studies of ice nucleation onto bare and internally mixed soot–sulfuric acid particles
  50. Measurement report: Introduction to the HyICE-2018 campaign for measurements of ice-nucleating particles and instrument inter-comparison in the Hyytiälä boreal forest
  51. Enhanced soot particle ice nucleation ability induced by aggregate compaction and densification
  52. Ice nucleating properties of aircraft turbine engine soot particles with respect to cirrus clouds formations
  53. Unveiling atmospheric transport and mixing mechanisms of ice-nucleating particles over the Alps
  54. Predicting atmospheric background number concentration of ice nucleating particles in the Arctic
  55. Retrieving ice nucleating particle concentration and ice multiplication factors using active remote sensing validated by in situ observations
  56. Homogeneous freezing of water droplets for different volumes and cooling rates
  57. The dependence of soot particle ice nucleation ability on its volatile content
  58. The contribution of Saharan dust to the ice-nucleating particle concentrations at the High Altitude Station Jungfraujoch (3580 m a.s.l.), Switzerland
  59. Enhanced soot particle ice nucleation ability induced by aggregate compaction and densification
  60. Sources and nature of ice-nucleating particles in the free troposphere at Jungfraujoch in winter 2017
  61. The diurnal and seasonal variability of ice nucleating particles at the High Altitude Station Jungfraujoch (3580 m a.s.l.), Switzerland
  62. Unveiling atmospheric transport and mixing mechanisms of ice nucleating particles over the Alps
  63. Ice nucleation activities of soot particles internally mixed with sulphuric acid at cirrus cloud conditions
  64. The contribution of Saharan dust to the ice nucleating particle concentrations at the High Altitude Station Jungfraujoch (3580 m a.s.l.), Switzerland
  65. On the drivers of droplet variability in alpine mixed-phase clouds
  66. The Role of Cloud Processing for the Ice Nucleating Ability of Organic Aerosol and Coal Fly Ash Particles
  67. Cloud from a chip: Quantifying the activity of ice-nucleating particles in microfluidic droplets
  68. Enhanced soot particle ice nucleation ability induced by aggregate compaction
  69. Towards parameterising atmospheric concentrations of ice-nucleating particles active at moderate supercooling
  70. Continuous online monitoring of ice-nucleating particles: development of the automated Horizontal Ice Nucleation Chamber (HINC-Auto)
  71. On the drivers of droplet variability in Alpine mixed-phase clouds
  72. Supplementary material to "On the drivers of droplet variability in Alpine mixed-phase clouds"
  73. Ice Nucleation Ability of Tree Pollen Altered by Atmospheric Processing
  74. Future warming exacerbated by aged-soot effect on cloud formation
  75. Continuous online-monitoring of Ice Nucleating Particles: development of the automated Horizontal Ice Nucleation Chamber (HINC-Auto)
  76. The role of contact angle and pore width on pore condensation and freezing
  77. Towards parametrising atmospheric concentrations of ice nucleating particles active at moderate supercooling
  78. Condensation/immersion mode ice-nucleating particles in a boreal environment
  79. Black Carbon Particles Do Not Matter for Immersion Mode Ice Nucleation
  80. New evidence of soot particles affecting past and future cloud formation and climate
  81. Aging induced changes in ice nucleation activity of combustion aerosol as determined by near edge X-ray absorption fine structure (NEXAFS) spectroscopy
  82. Development of the DRoplet Ice Nuclei Counter Zurich (DRINCZ): validation and application to field-collected snow samples
  83. Ice-nucleating particle versus ice crystal number concentrationin altocumulus and cirrus layers embedded in Saharan dust:a closure study
  84. The Role of Contact Angle and Pore Width on Pore Condensation and Freezing
  85. Photomineralization mechanism changes the ability of dissolved organic matter to activate cloud droplets and to nucleate ice crystals
  86. Ice nucleation properties of K-feldspar polymorphs and plagioclase feldspars
  87. The Impact of Cloud Processing on the Ice Nucleation Abilities of Soot Particles at Cirrus Temperatures
  88. Ice nucleation properties of K-feldspar polymorphs and plagioclase feldspars
  89. Ice nucleation properties of K-feldspar polymorphs and plagioclase feldspars
  90. A high-speed particle phase discriminator (PPD-HS) for the classification of airborne particles, as tested in a continuous flow diffusion chamber
  91. Field evaluation of a Portable Fine Particle Concentrator (PFPC) for ice nucleating particle measurements
  92. Ice-nucleating particle versus ice crystal number concentration in altocumulus and cirrus embedded in Saharan dust: A closure study
  93. Photomineralization mechanism changes the ability of dissolved organic matter to activate cloud droplets and to nucleate ice crystals
  94. Supplementary material to "Photomineralization mechanism changes the ability of dissolved organic matter to activate cloud droplets and to nucleate ice crystals"
  95. Heterogeneous ice nucleation properties of natural desert dust particles coated with a surrogate of secondary organic aerosol
  96. Pore condensation and freezing is responsible for ice formation below water saturation for porous particles
  97. Heterogeneous Ice Nucleation Properties of Natural Desert Dust Particles Coated with a Surrogate of Secondary Organic Aerosol
  98. Heterogeneous Ice Nucleation Properties of Natural Desert Dust Particles Coated with a Surrogate of Secondary Organic Aerosol
  99. A High Speed Particle Phase Discriminator (PPD-HS) for the classification of airborne particles, as tested in a continuous flow diffusion chamber
  100. A High Speed Particle Phase Discriminator (PPD-HS) for the classification of airborne particles, as tested in a continuous flow diffusion chamber
  101. Heterogeneous ice nucleation on dust particles sourced from nine deserts worldwide – Part 2: Deposition nucleation and condensation freezing
  102. Ice nucleation properties of K-feldspar polymorphs and plagioclase feldspars
  103. A laboratory investigation of the ice nucleation efficiency of three types of mineral and soil dust
  104. The Fifth International Workshop on Ice Nucleation phase 2 (FIN-02): laboratory intercomparison of ice nucleation measurements
  105. Heterogeneous ice nucleation on dust particles sourced from 9 deserts worldwide – Part 2: Deposition nucleation and condensation freezing
  106. Ice nucleation abilities of soot particles determined with the Horizontal Ice Nucleation Chamber
  107. Impact of Air Mass Conditions and Aerosol Properties on Ice Nucleating Particle Concentrations at the High Altitude Research Station Jungfraujoch
  108. Background Free-Tropospheric Ice Nucleating Particle Concentrations at Mixed-Phase Cloud Conditions
  109. Heterogeneous Ice Nucleation Properties of Natural Desert Dust Particles Coated with a Surrogate of Secondary Organic Aerosol
  110. The Fifth International Workshop on Ice Nucleation phase 2 (FIN-02): Laboratory intercomparison of ice nucleation measurements
  111. A laboratory investigation of the ice nucleation efficiency of three types of mineral and soil dust
  112. Marine and Terrestrial Organic Ice-Nucleating Particles in Pristine Marine to Continentally Influenced Northeast Atlantic Air Masses
  113. Ice nucleation abilities of soot particles determined with the Horizontal Ice Nucleation Chamber
  114. Ice nucleation abilities of soot particles determined with the Horizontal Ice Nucleation Chamber
  115. The Horizontal Ice Nucleation Chamber (HINC): INP measurements at conditions relevant for mixed-phase clouds at the High Altitude Research Station Jungfraujoch
  116. Leipzig Ice Nucleation chamber Comparison (LINC): intercomparison of four online ice nucleation counters
  117. Uncertainty in counting ice nucleating particles with continuous flow diffusion chambers
  118. Perspectives on the Future of Ice Nucleation Research: Research Needs and Unanswered Questions Identified from Two International Workshops
  119. The Horizontal Ice Nucleation Chamber HINC: INP measurements at Conditions Relevant for Mixed-Phase Clouds at the High Altitude Research Station Jungfraujoch
  120. Leipzig Ice Nucleation chamber Comparison (LINC): Inter-comparison of four online ice nucleation counters
  121. Uncertainty in counting ice nucleating particles with continuous diffusion flow chambers
  122. Overview of Ice Nucleating Particles
  123. Measurements of Ice Nucleating Particles and Ice Residuals
  124. Heterogeneous ice nucleation on dust particles sourced from nine deserts worldwide – Part 1: Immersion freezing
  125. Chapter 7. Secondary Ice Production - current state of the science and recommendations for the future
  126. Persistence of orographic mixed-phase clouds
  127. Ice nucleating particles in the Saharan Air Layer
  128. Heterogeneous ice nucleation on dust particles sourced from 9 deserts worldwide – Part 1: Immersion freezing
  129. Heterogeneous ice nucleation on dust particles sourced from 9 deserts worldwide – Part 1: Immersion freezing
  130. Immersion mode ice nucleation measurements with the new Portable Immersion Mode Cooling chAmber (PIMCA)
  131. Ice Nucleating Particle Measurements at 241 K during Winter Months at 3580 m MSL in the Swiss Alps
  132. Ice nucleating particles in the Saharan Air Layer
  133. Ice nucleating particles in the Saharan Air Layer
  134. A comprehensive laboratory study on the immersion freezing behavior of illite NX particles: a comparison of 17 ice nucleation measurement techniques
  135. Intercomparing different devices for the investigation of ice nucleating particles using Snomax<sup>®</sup> as test substance
  136. Exploring the Mechanisms of Ice Nucleation on Kaolinite: From Deposition Nucleation to Condensation Freezing
  137. Laboratory studies of immersion and deposition mode ice nucleation of ozone aged mineral dust particles
  138. Laboratory studies of immersion and deposition mode ice nucleation of ozone aged mineral dust particles
  139. Effect of photochemical ageing on the ice nucleation properties of diesel and wood burning particles
  140. Heterogeneous ice nucleation of mineral dust particles exposed to ozone
  141. Immersion freezing of clay minerals and bacterial ice nuclei
  142. Time dependence of immersion freezing: an experimental study on size selected kaolinite particles
  143. Resurgence in Ice Nuclei Measurement Research
  144. Ice nuclei properties within a Saharan dust event at the Jungfraujoch in the Swiss Alps
  145. Results from the University of Toronto continuous flow diffusion chamber at ICIS 2007: instrument intercomparison and ice onsets for different aerosol types
  146. Ice Nucleation onto Arizona Test Dust at Cirrus Temperatures: Effect of Temperature and Aerosol Size on Onset Relative Humidity
  147. The University of Toronto Continuous Flow Diffusion Chamber (UT-CFDC): A Simple Design for Ice Nucleation Studies
  148. Ice formation via deposition nucleation on mineral dust and organics: dependence of onset relative humidity on total particulate surface area
  149. Solid Ammonium Sulfate Aerosols as Ice Nuclei: A Pathway for Cirrus Cloud Formation
  150. Laboratory studies of ice formation via deposition mode nucleation onto mineral dust and n-hexane soot samples
  151. Aging Effects on Oxidized and Amine-Modified Poly(dimethylsiloxane) Surfaces Studied with Chemical Force Titrations:  Effects on Electroosmotic Flow Rate in Microfluidic Channels
  152. Surface characterization using chemical force microscopy and the flow performance of modified polydimethylsiloxane for microfluidic device applications