Aerosol indirect effect from turbulence-induced broadening of cloud-droplet size distributions
Abstract
Here, the influence of aerosol concentration on cloud droplet size distribution is investigated in a laboratory chamber that enables turbulent cloud formation through moist convection. The experiments allow steady-state microphysics to be achieved, with aerosol input balanced by cloud droplet growth and fallout. As aerosol concentration is increased the cloud droplet mean diameter decreases as expected, but the width of the size distribution also decreases sharply. The aerosol input allows for cloud generation in the limiting regimes of fast microphysics (τc < τt) for high aerosol concentration, and slow microphysics (τc > τt) for low aerosol concentration; here, τc is the phase relaxation time and τt is the turbulence correlation time. The increase in the width of the droplet size distribution for the low aerosol limit is consistent with larger variability of supersaturation due to the slow microphysical response. A stochastic differential equation for supersaturation predicts that the standard deviation of the squared droplet radius should increase linearly with a system time scale defined as τs-1 =τc-1 + τt-1, and the measurements are in excellent agreement with this finding. This finding underscores the importance of droplet size dispersion for the aerosol indirect effect: increasing aerosol concentration not only suppresses precipitationmore »
- Authors:
- Publication Date:
- Research Org.:
- Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
- Sponsoring Org.:
- USDOE
- OSTI Identifier:
- 1333749
- Alternate Identifier(s):
- OSTI ID: 1340762
- Report Number(s):
- PNNL-SA-119793
Journal ID: ISSN 0027-8424
- Grant/Contract Number:
- AC06-76RL01830; AC05-76RL01830
- Resource Type:
- Published Article
- Journal Name:
- Proceedings of the National Academy of Sciences of the United States of America
- Additional Journal Information:
- Journal Name: Proceedings of the National Academy of Sciences of the United States of America Journal Volume: 113 Journal Issue: 50; Journal ID: ISSN 0027-8424
- Publisher:
- National Academy of Sciences, Washington, DC (United States)
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; aerosol indirect effect; cloud-droplet size distribution; cloud–turbulence interactions
Citation Formats
Chandrakar, Kamal Kant, Cantrell, Will, Chang, Kelken, Ciochetto, David, Niedermeier, Dennis, Ovchinnikov, Mikhail, Shaw, Raymond A., and Yang, Fan. Aerosol indirect effect from turbulence-induced broadening of cloud-droplet size distributions. United States: N. p., 2016.
Web. doi:10.1073/pnas.1612686113.
Chandrakar, Kamal Kant, Cantrell, Will, Chang, Kelken, Ciochetto, David, Niedermeier, Dennis, Ovchinnikov, Mikhail, Shaw, Raymond A., & Yang, Fan. Aerosol indirect effect from turbulence-induced broadening of cloud-droplet size distributions. United States. https://doi.org/10.1073/pnas.1612686113
Chandrakar, Kamal Kant, Cantrell, Will, Chang, Kelken, Ciochetto, David, Niedermeier, Dennis, Ovchinnikov, Mikhail, Shaw, Raymond A., and Yang, Fan. Mon .
"Aerosol indirect effect from turbulence-induced broadening of cloud-droplet size distributions". United States. https://doi.org/10.1073/pnas.1612686113.
@article{osti_1333749,
title = {Aerosol indirect effect from turbulence-induced broadening of cloud-droplet size distributions},
author = {Chandrakar, Kamal Kant and Cantrell, Will and Chang, Kelken and Ciochetto, David and Niedermeier, Dennis and Ovchinnikov, Mikhail and Shaw, Raymond A. and Yang, Fan},
abstractNote = {Here, the influence of aerosol concentration on cloud droplet size distribution is investigated in a laboratory chamber that enables turbulent cloud formation through moist convection. The experiments allow steady-state microphysics to be achieved, with aerosol input balanced by cloud droplet growth and fallout. As aerosol concentration is increased the cloud droplet mean diameter decreases as expected, but the width of the size distribution also decreases sharply. The aerosol input allows for cloud generation in the limiting regimes of fast microphysics (τc < τt) for high aerosol concentration, and slow microphysics (τc > τt) for low aerosol concentration; here, τc is the phase relaxation time and τt is the turbulence correlation time. The increase in the width of the droplet size distribution for the low aerosol limit is consistent with larger variability of supersaturation due to the slow microphysical response. A stochastic differential equation for supersaturation predicts that the standard deviation of the squared droplet radius should increase linearly with a system time scale defined as τs-1 =τc-1 + τt-1, and the measurements are in excellent agreement with this finding. This finding underscores the importance of droplet size dispersion for the aerosol indirect effect: increasing aerosol concentration not only suppresses precipitation formation through reduction of the mean droplet diameter, but perhaps more importantly, through narrowing of the droplet size distribution due to reduced supersaturation fluctuations. Supersaturation fluctuations in the low aerosol / slow microphysics limit are likely of leading importance for precipitation formation.},
doi = {10.1073/pnas.1612686113},
journal = {Proceedings of the National Academy of Sciences of the United States of America},
number = 50,
volume = 113,
place = {United States},
year = {Mon Nov 28 00:00:00 EST 2016},
month = {Mon Nov 28 00:00:00 EST 2016}
}
https://doi.org/10.1073/pnas.1612686113
Web of Science
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