Articles | Volume 16, issue 22
Atmos. Chem. Phys., 16, 14317–14329, 2016
https://doi.org/10.5194/acp-16-14317-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 16, 14317–14329, 2016
https://doi.org/10.5194/acp-16-14317-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article 17 Nov 2016
Research article | 17 Nov 2016
Application of a new scheme of cloud base droplet nucleation in a spectral (bin) microphysics cloud model: sensitivity to aerosol size distribution
Eyal Ilotoviz and Alexander Khain
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Cited
9 citations as recorded by crossref.
- Calculation of supersaturation maximum and droplet concentration at cloud boundaries M. Pinsky & A. Khain 10.1016/j.atmosres.2019.104694
- The Role of Ice Splintering on Microphysics of Deep Convective Clouds Forming Under Different Aerosol Conditions: Simulations Using the Model With Spectral Bin Microphysics Y. Qu et al. 10.1029/2019JD031312
- Effects of Anthropogenic Aerosols on a Heavy Rainstorm in Beijing C. Guo et al. 10.3390/atmos10040162
- Simulating a Mesoscale Convective System Using WRF With a New Spectral Bin Microphysics: 1: Hail vs Graupel J. Shpund et al. 10.1029/2019JD030576
- The Roles of Mineral Dust as Cloud Condensation Nuclei and Ice Nuclei During the Evolution of a Hail Storm Q. Chen et al. 10.1029/2019JD031403
- Empirical values and assumptions in the microphysics of numerical models F. Tapiador et al. 10.1016/j.atmosres.2018.09.010
- Saharan Dust Aerosols Change Deep Convective Cloud Prevalence, Possibly by Inhibiting Marine New Particle Formation L. Zamora & R. Kahn 10.1175/JCLI-D-20-0083.1
- Relationship between Aerosols, Hail Microphysics, and ZDR Columns E. Ilotoviz et al. 10.1175/JAS-D-17-0127.1
- Droplet growth during vapor-liquid transition in a 2D Lennard-Jones fluid J. Midya & S. Das 10.1063/1.4973617
8 citations as recorded by crossref.
- Calculation of supersaturation maximum and droplet concentration at cloud boundaries M. Pinsky & A. Khain 10.1016/j.atmosres.2019.104694
- The Role of Ice Splintering on Microphysics of Deep Convective Clouds Forming Under Different Aerosol Conditions: Simulations Using the Model With Spectral Bin Microphysics Y. Qu et al. 10.1029/2019JD031312
- Effects of Anthropogenic Aerosols on a Heavy Rainstorm in Beijing C. Guo et al. 10.3390/atmos10040162
- Simulating a Mesoscale Convective System Using WRF With a New Spectral Bin Microphysics: 1: Hail vs Graupel J. Shpund et al. 10.1029/2019JD030576
- The Roles of Mineral Dust as Cloud Condensation Nuclei and Ice Nuclei During the Evolution of a Hail Storm Q. Chen et al. 10.1029/2019JD031403
- Empirical values and assumptions in the microphysics of numerical models F. Tapiador et al. 10.1016/j.atmosres.2018.09.010
- Saharan Dust Aerosols Change Deep Convective Cloud Prevalence, Possibly by Inhibiting Marine New Particle Formation L. Zamora & R. Kahn 10.1175/JCLI-D-20-0083.1
- Relationship between Aerosols, Hail Microphysics, and ZDR Columns E. Ilotoviz et al. 10.1175/JAS-D-17-0127.1
1 citations as recorded by crossref.
Latest update: 17 Sep 2021
Short summary
In this paper the evolution of deep convective clouds is simulated under different aerosol loading. The simulations are performed using a spectral-bin microphysics model in which droplet concentration at cloud base is calculated using a new analytical method. The effect of this accurate calculation of droplet concentration is analyzed by comparison with a standard method. The role of the smallest CCN in the aerosol spectra is investigated.
In this paper the evolution of deep convective clouds is simulated under different aerosol...
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