Articles | Volume 23, issue 9
https://doi.org/10.5194/acp-23-5217-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-23-5217-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Mixed-phase direct numerical simulation: ice growth in cloud-top generating cells
National Center for Atmospheric Research (NCAR), Boulder, CO, USA
Lulin Xue
National Center for Atmospheric Research (NCAR), Boulder, CO, USA
Sarah Tessendorf
National Center for Atmospheric Research (NCAR), Boulder, CO, USA
Kyoko Ikeda
National Center for Atmospheric Research (NCAR), Boulder, CO, USA
Courtney Weeks
National Center for Atmospheric Research (NCAR), Boulder, CO, USA
Roy Rasmussen
National Center for Atmospheric Research (NCAR), Boulder, CO, USA
Melvin Kunkel
Idaho Power Company, Boise, ID, USA
Derek Blestrud
Idaho Power Company, Boise, ID, USA
Shaun Parkinson
Idaho Power Company, Boise, ID, USA
Melinda Meadows
Idaho Power Company, Boise, ID, USA
Nick Dawson
Idaho Power Company, Boise, ID, USA
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This study employs a parcel–DNS (direct numerical simulation) modeling framework to accurately resolve the aerosol–droplet–turbulence interactions in an ascending air parcel. The effect of turbulence, aerosol hygroscopicity, and aerosol mass loading on droplet growth and rain formation is investigated through a series of in-cloud seeding experiments in which hygroscopic particles were seeded near the cloud base.
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Short summary
The possible mechanism of effective ice growth in the cloud-top generating cells in winter orographic clouds is explored using a newly developed ultra-high-resolution cloud microphysics model. Simulations demonstrate that a high availability of moisture and liquid water is critical for producing large ice particles. Fluctuations in temperature and moisture down to millimeter scales due to cloud turbulence can substantially affect the growth history of the individual cloud particles.
The possible mechanism of effective ice growth in the cloud-top generating cells in winter...
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