Laboratory Investigations of Aerosol-Cloud Interactions in an Entraining, Turbulent Environment
Principal Investigator
Will Cantrell
— Michigan Technological University
Abstract
Every cloud droplet in Earth’s atmosphere formed on a preexisting mote of dust – an aerosol particle. Such aerosol-cloud interactions are crucial elements of Earth’s climate system, and they must be understood and reliably represented in models of the atmosphere (for example, for predicting weather). One of the factors that governs how aerosol particles determine cloud properties is how clouds mix with surrounding air, a process called entrainment. We propose to conduct laboratory experiments of aerosol-cloud interactions in a setting in which we can measure the effects of entrainment. Preliminary results from our novel experimental facility, Michigan Technological University’s Pi Chamber, show that as the fraction of air that is mixed into the cloud increases, the width of the cloud droplet size distribution increases, and the fraction of aerosol particles that become cloud droplets decreases. These two effects have implications for the formation of precipitation. We will conduct measurements of the effects of entrainment on aerosol-cloud interactions in this laboratory setting where we can control and verify entrainment independently. We will use a large eddy simulation model that we have developed for the chamber to investigate processes that we cannot directly measure. Finally, we will compare data from these experiments and simulations to data from field campaigns where entrainment is suspected to be playing a role.
Related Publications
Yeom J, H Fahandezh Sadi, J Anderson, F Yang, W Cantrell, and R Shaw. 2025. "Cloud microphysical response to entrainment of dry air containing aerosols." npj Climate and Atmospheric Science, 8(1), 10.1038/s41612-024-00889-7.
Wang A, M Ovchinnikov, F Yang, W Cantrell, J Yeom, and R Shaw. 2024. "The Dual Nature of Entrainment-Mixing Signatures Revealed through Large-Eddy Simulations of a Convection-Cloud Chamber." Journal of the Atmospheric Sciences, 81(12), 10.1175/JAS-D-24-0043.1.
Anderson J, I Helman, R Shaw, and W Cantrell. 2024. "Droplet Growth or Evaporation Does Not Buffer the Variability in Supersaturation in Clean Clouds." Journal of the Atmospheric Sciences, 81(1), 10.1175/JAS-D-23-0104.1.
Yeom J, I Helman, P Prabhakaran, J Anderson, F Yang, R Shaw, and W Cantrell. 2023. "Cloud microphysical response to entrainment and mixing is locally inhomogeneous and globally homogeneous: Evidence from the lab." Proceedings of the National Academy of Sciences, 120(42), e2307354120, 10.1073/pnas.2307354120.