Articles | Volume 18, issue 22
https://doi.org/10.5194/acp-18-16461-2018
© Author(s) 2018. 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-18-16461-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The effect of secondary ice production parameterization on the simulation of a cold frontal rainband
Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
Department of Chemical and Biomolecular Engineering, Georgia Institute of Technology, Atlanta, GA 30332, USA
Christian Barthlott
Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
Jonathan Crosier
School of Earth, Atmospheric, and Environmental Studies, University of Manchester, Manchester, UK
Ilya Zhukov
Jülich Supercomputing Center, Forschungszentrum Jülich, Jülich, Germany
Athanasios Nenes
CORRESPONDING AUTHOR
Department of Chemical and Biomolecular Engineering, Georgia Institute of Technology, Atlanta, GA 30332, USA
ICE-HT, Foundation for Research and Technology, Hellas, 26504 Patras, Greece
Institute of Environmental Research and Sustainable Development, National Observatory of Athens, 15236 Palea Penteli, Greece
Laboratory of Atmospheric Processes and their Impacts, School of Architecture, Civil and Environmental Engineering, École Polytechnique Fédérale de Lausanne, CH 1015, Lausanne,
Switzerland
Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
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Cited
19 citations as recorded by crossref.
- New type of evidence for secondary ice formation at around −15 °C in mixed-phase clouds C. Mignani et al. 10.5194/acp-19-877-2019
- Two-year statistics of columnar-ice production in stratiform clouds over Hyytiälä, Finland: environmental conditions and the relevance to secondary ice production H. Li et al. 10.5194/acp-21-14671-2021
- The impact of secondary ice production on Arctic stratocumulus G. Sotiropoulou et al. 10.5194/acp-20-1301-2020
- Secondary Ice Formation in Idealised Deep Convection—Source of Primary Ice and Impact on Glaciation A. Miltenberger et al. 10.3390/atmos11050542
- Ice multiplication from ice–ice collisions in the high Arctic: sensitivity to ice habit, rimed fraction, ice type and uncertainties in the numerical description of the process G. Sotiropoulou et al. 10.5194/acp-21-9741-2021
- Secondary ice production in summer clouds over the Antarctic coast: an underappreciated process in atmospheric models G. Sotiropoulou et al. 10.5194/acp-21-755-2021
- Heavy snowfall event over the Swiss Alps: did wind shear impact secondary ice production? Z. Dedekind et al. 10.5194/acp-23-2345-2023
- Impacts of secondary ice production on Arctic mixed-phase clouds based on ARM observations and CAM6 single-column model simulations X. Zhao et al. 10.5194/acp-21-5685-2021
- Sensitivity of cloud-phase distribution to cloud microphysics and thermodynamics in simulated deep convective clouds and SEVIRI retrievals C. Han et al. 10.5194/acp-23-14077-2023
- How frequent is natural cloud seeding from ice cloud layers ( < −35 °C) over Switzerland? U. Proske et al. 10.5194/acp-21-5195-2021
- Simulating the seeder–feeder impacts on cloud ice and precipitation over the Alps Z. Dedekind et al. 10.5194/acp-24-5389-2024
- Effects of secondary ice processes on a stratocumulus to cumulus transition during a cold-air outbreak M. Karalis et al. 10.1016/j.atmosres.2022.106302
- Continuous secondary-ice production initiated by updrafts through the melting layer in mountainous regions A. Lauber et al. 10.5194/acp-21-3855-2021
- Cold cloud microphysical process rates in a global chemistry–climate model S. Bacer et al. 10.5194/acp-21-1485-2021
- Secondary ice production processes in wintertime alpine mixed-phase clouds P. Georgakaki et al. 10.5194/acp-22-1965-2022
- Sensitivity of precipitation formation to secondary ice production in winter orographic mixed-phase clouds Z. Dedekind et al. 10.5194/acp-21-15115-2021
- New insights into ice multiplication using remote-sensing observations of slightly supercooled mixed-phase clouds in the Arctic E. Luke et al. 10.1073/pnas.2021387118
- On the drivers of droplet variability in alpine mixed-phase clouds P. Georgakaki et al. 10.5194/acp-21-10993-2021
- Microphysical processes producing high ice water contents (HIWCs) in tropical convective clouds during the HAIC-HIWC field campaign: dominant role of secondary ice production Y. Huang et al. 10.5194/acp-22-2365-2022
19 citations as recorded by crossref.
- New type of evidence for secondary ice formation at around −15 °C in mixed-phase clouds C. Mignani et al. 10.5194/acp-19-877-2019
- Two-year statistics of columnar-ice production in stratiform clouds over Hyytiälä, Finland: environmental conditions and the relevance to secondary ice production H. Li et al. 10.5194/acp-21-14671-2021
- The impact of secondary ice production on Arctic stratocumulus G. Sotiropoulou et al. 10.5194/acp-20-1301-2020
- Secondary Ice Formation in Idealised Deep Convection—Source of Primary Ice and Impact on Glaciation A. Miltenberger et al. 10.3390/atmos11050542
- Ice multiplication from ice–ice collisions in the high Arctic: sensitivity to ice habit, rimed fraction, ice type and uncertainties in the numerical description of the process G. Sotiropoulou et al. 10.5194/acp-21-9741-2021
- Secondary ice production in summer clouds over the Antarctic coast: an underappreciated process in atmospheric models G. Sotiropoulou et al. 10.5194/acp-21-755-2021
- Heavy snowfall event over the Swiss Alps: did wind shear impact secondary ice production? Z. Dedekind et al. 10.5194/acp-23-2345-2023
- Impacts of secondary ice production on Arctic mixed-phase clouds based on ARM observations and CAM6 single-column model simulations X. Zhao et al. 10.5194/acp-21-5685-2021
- Sensitivity of cloud-phase distribution to cloud microphysics and thermodynamics in simulated deep convective clouds and SEVIRI retrievals C. Han et al. 10.5194/acp-23-14077-2023
- How frequent is natural cloud seeding from ice cloud layers ( < −35 °C) over Switzerland? U. Proske et al. 10.5194/acp-21-5195-2021
- Simulating the seeder–feeder impacts on cloud ice and precipitation over the Alps Z. Dedekind et al. 10.5194/acp-24-5389-2024
- Effects of secondary ice processes on a stratocumulus to cumulus transition during a cold-air outbreak M. Karalis et al. 10.1016/j.atmosres.2022.106302
- Continuous secondary-ice production initiated by updrafts through the melting layer in mountainous regions A. Lauber et al. 10.5194/acp-21-3855-2021
- Cold cloud microphysical process rates in a global chemistry–climate model S. Bacer et al. 10.5194/acp-21-1485-2021
- Secondary ice production processes in wintertime alpine mixed-phase clouds P. Georgakaki et al. 10.5194/acp-22-1965-2022
- Sensitivity of precipitation formation to secondary ice production in winter orographic mixed-phase clouds Z. Dedekind et al. 10.5194/acp-21-15115-2021
- New insights into ice multiplication using remote-sensing observations of slightly supercooled mixed-phase clouds in the Arctic E. Luke et al. 10.1073/pnas.2021387118
- On the drivers of droplet variability in alpine mixed-phase clouds P. Georgakaki et al. 10.5194/acp-21-10993-2021
- Microphysical processes producing high ice water contents (HIWCs) in tropical convective clouds during the HAIC-HIWC field campaign: dominant role of secondary ice production Y. Huang et al. 10.5194/acp-22-2365-2022
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Short summary
Ice crystal formation in clouds can occur via thermodynamic nucleation, but also via mechanical collisions between pre-existing crystals or co-existing droplets. When descriptions of this mechanical ice generation are implemented into the COSMO weather model, we find that the contributions to crystal number from thermodynamic and mechanical processes are of the same order. Mechanical ice generation also intensifies differences in precipitation intensity between dynamic and quiescent regions.
Ice crystal formation in clouds can occur via thermodynamic nucleation, but also via mechanical...
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