Articles | Volume 16, issue 14
https://doi.org/10.5194/acp-16-9421-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-9421-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
29 Jul 2016
Research article |
| 29 Jul 2016
Conditions for super-adiabatic droplet growth after entrainment mixing
Fan Yang
Atmospheric Sciences Program and Department of Physics, Michigan Technological University, Houghton, Michigan, USA
Atmospheric Sciences Program and Department of Physics, Michigan Technological University, Houghton, Michigan, USA
Huiwen Xue
Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, China
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Cited
22 citations as recorded by crossref.
- Role of droplet size classes on the cloud droplet spectral dispersion as observed over the Western Ghats K. Ansari et al. 10.1016/j.atmosres.2020.105104
- Parameterizations of Entrainment‐Mixing Mechanisms and Their Effects on Cloud Droplet Spectral Width Based on Numerical Simulations S. Luo et al. 10.1029/2020JD032972
- A new methodology for the statistical descriptions of Particle‐by‐Particle measurements of liquid droplets in cumulus clouds S. Bera et al. 10.1002/qj.4234
- Relationship between Turbulence and Drizzle in Continental and Marine Low Stratiform Clouds P. Borque et al. 10.1175/JAS-D-18-0060.1
- Aerosol indirect effect from turbulence-induced broadening of cloud-droplet size distributions K. Chandrakar et al. 10.1073/pnas.1612686113
- Consideration of Initial Cloud Droplet Size Distribution Shapes in Quantifying Different Entrainment‐Mixing Mechanisms S. Luo et al. 10.1029/2020JD034455
- Physical Interpretation of Mixing Diagrams A. Khain et al. 10.1002/2017JD027124
- Revisiting adiabatic fraction estimations in cumulus clouds: high-resolution simulations with a passive tracer E. Eytan et al. 10.5194/acp-21-16203-2021
- An Intercomparison of Large‐Eddy Simulations of a Convection Cloud Chamber Using Haze‐Capable Bin and Lagrangian Cloud Microphysics Schemes F. Yang et al. 10.1029/2022MS003270
- Supersaturation Fluctuations during the Early Stage of Cumulus Formation H. Siebert & R. Shaw 10.1175/JAS-D-16-0115.1
- Drop Size Distribution Broadening Mechanisms in a Bin Microphysics Eulerian Model L. Pardo et al. 10.1175/JAS-D-20-0099.1
- Vertical Variation of Turbulent Entrainment Mixing Processes in Marine Stratocumulus Clouds Using High‐Resolution Digital Holography N. Desai et al. 10.1029/2020JD033527
- Theoretical analysis of mixing in liquid clouds – Part IV: DSD evolution and mixing diagrams M. Pinsky & A. Khain 10.5194/acp-18-3659-2018
- Broadening of cloud droplet size distributions and warm rain initiation associated with turbulence: an overview C. LU et al. 10.1080/16742834.2018.1410057
- Search for Microphysical Signatures of Stochastic Condensation in Marine Boundary Layer Clouds Using Airborne Digital Holography N. Desai et al. 10.1029/2018JD029033
- Contrasting Scale Dependence of Entrainment‐Mixing Mechanisms in Stratocumulus Clouds S. Gao et al. 10.1029/2020GL086970
- Shallow Cumulus Properties as Captured by Adiabatic Fraction in High-Resolution LES Simulations E. Eytan et al. 10.1175/JAS-D-21-0201.1
- Cloud droplet size distribution broadening during diffusional growth: ripening amplified by deactivation and reactivation F. Yang et al. 10.5194/acp-18-7313-2018
- Observational study of the relationship between entrainment rate and relative dispersion in deep convective clouds X. Guo et al. 10.1016/j.atmosres.2017.09.013
- Scale Dependence of Cloud Microphysical Response to Turbulent Entrainment and Mixing B. Kumar et al. 10.1029/2018MS001487
- Observational Relationship Between Entrainment Rate and Environmental Relative Humidity and Implications for Convection Parameterization C. Lu et al. 10.1029/2018GL080264
- Influences of an entrainment–mixing parameterization on numerical simulations of cumulus and stratocumulus clouds X. Xu et al. 10.5194/acp-22-5459-2022
22 citations as recorded by crossref.
- Role of droplet size classes on the cloud droplet spectral dispersion as observed over the Western Ghats K. Ansari et al. 10.1016/j.atmosres.2020.105104
- Parameterizations of Entrainment‐Mixing Mechanisms and Their Effects on Cloud Droplet Spectral Width Based on Numerical Simulations S. Luo et al. 10.1029/2020JD032972
- A new methodology for the statistical descriptions of Particle‐by‐Particle measurements of liquid droplets in cumulus clouds S. Bera et al. 10.1002/qj.4234
- Relationship between Turbulence and Drizzle in Continental and Marine Low Stratiform Clouds P. Borque et al. 10.1175/JAS-D-18-0060.1
- Aerosol indirect effect from turbulence-induced broadening of cloud-droplet size distributions K. Chandrakar et al. 10.1073/pnas.1612686113
- Consideration of Initial Cloud Droplet Size Distribution Shapes in Quantifying Different Entrainment‐Mixing Mechanisms S. Luo et al. 10.1029/2020JD034455
- Physical Interpretation of Mixing Diagrams A. Khain et al. 10.1002/2017JD027124
- Revisiting adiabatic fraction estimations in cumulus clouds: high-resolution simulations with a passive tracer E. Eytan et al. 10.5194/acp-21-16203-2021
- An Intercomparison of Large‐Eddy Simulations of a Convection Cloud Chamber Using Haze‐Capable Bin and Lagrangian Cloud Microphysics Schemes F. Yang et al. 10.1029/2022MS003270
- Supersaturation Fluctuations during the Early Stage of Cumulus Formation H. Siebert & R. Shaw 10.1175/JAS-D-16-0115.1
- Drop Size Distribution Broadening Mechanisms in a Bin Microphysics Eulerian Model L. Pardo et al. 10.1175/JAS-D-20-0099.1
- Vertical Variation of Turbulent Entrainment Mixing Processes in Marine Stratocumulus Clouds Using High‐Resolution Digital Holography N. Desai et al. 10.1029/2020JD033527
- Theoretical analysis of mixing in liquid clouds – Part IV: DSD evolution and mixing diagrams M. Pinsky & A. Khain 10.5194/acp-18-3659-2018
- Broadening of cloud droplet size distributions and warm rain initiation associated with turbulence: an overview C. LU et al. 10.1080/16742834.2018.1410057
- Search for Microphysical Signatures of Stochastic Condensation in Marine Boundary Layer Clouds Using Airborne Digital Holography N. Desai et al. 10.1029/2018JD029033
- Contrasting Scale Dependence of Entrainment‐Mixing Mechanisms in Stratocumulus Clouds S. Gao et al. 10.1029/2020GL086970
- Shallow Cumulus Properties as Captured by Adiabatic Fraction in High-Resolution LES Simulations E. Eytan et al. 10.1175/JAS-D-21-0201.1
- Cloud droplet size distribution broadening during diffusional growth: ripening amplified by deactivation and reactivation F. Yang et al. 10.5194/acp-18-7313-2018
- Observational study of the relationship between entrainment rate and relative dispersion in deep convective clouds X. Guo et al. 10.1016/j.atmosres.2017.09.013
- Scale Dependence of Cloud Microphysical Response to Turbulent Entrainment and Mixing B. Kumar et al. 10.1029/2018MS001487
- Observational Relationship Between Entrainment Rate and Environmental Relative Humidity and Implications for Convection Parameterization C. Lu et al. 10.1029/2018GL080264
- Influences of an entrainment–mixing parameterization on numerical simulations of cumulus and stratocumulus clouds X. Xu et al. 10.5194/acp-22-5459-2022
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Latest update: 24 Apr 2024
Short summary
When dry air is mixed into a cloud, droplets evaporate. If the diluted cloud mixture continues to rise, the remaining droplets will grow. In this work we show theoretically and computationally that a critical height exists, above which the droplets in a mixed, diluted cloud volume become larger than those in an undiluted volume. An environment that is humid and aerosol free is most favorable for producing such large droplets, which may contribute to the onset of precipitation formation.
When dry air is mixed into a cloud, droplets evaporate. If the diluted cloud mixture continues...
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