Aerosol partitioning between the interstitial and the condensed phase in mixed‐phase clouds

Type
01A - Journal article
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Parent work
Journal of Geophysical Research: Atmospheres
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DOI of the original publication
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Volume
112
Issue / Number
D23
Pages / Duration
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Publisher / Publishing institution
Wiley
Place of publication / Event location
Hoboken
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Abstract
The partitioning of aerosol particles between the cloud and the interstitial phase (i.e., unactivated aerosol) has been investigated during several Cloud and Aerosol Characterization Experiments (CLACE‐3, CLACE‐3½ and CLACE‐4) conducted in winter and summer 2004 and winter 2005 at the high alpine research station Jungfraujoch (3580 m altitude, Switzerland). Ambient air was sampled using different inlets in order to determine the activated fraction of aerosol particles, FN, defined as the fraction of the total aerosol number concentration (with particle diameter dp > 100 nm) that has been incorporated into cloud particles. The liquid and ice water content of mixed‐phase clouds were characterized by analyzing multiple cloud probes. The dependence of the activated fraction on several environmental factors is discussed on the basis of more than 900 h of in‐cloud observations and parameterizations for key variables are given. FN is found to increase with increasing liquid water content and to decrease with increasing particle number concentration in liquid clouds. FN also decreases with increasing cloud ice mass fraction and with decreasing temperature from 0 to −25°C. The Wegener‐Bergeron‐Findeisen process probably contributed to this trend, since the presence of ice crystals causes liquid droplets to evaporate, thus releasing the formerly activated particles back into the interstitial phase. Ice nucleation could also have prevented additional cloud condensation nuclei from activating. The observed activation behavior has significant implications for our understanding of the indirect effect of aerosols on climate.
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ISBN
ISSN
2169-8996
2169-897X
10.1029/2007jd008714
Language
English
Created during FHNW affiliation
No
Strategic action fields FHNW
Publication status
Published
Review
Peer review of the complete publication
Open access category
Closed
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Citation
Verheggen, B., Cozic, J., Weingartner, E., Bower, K., Mertes, S., Connolly, P., Gallagher, M., Flynn, M., Choularton, T., & Baltensperger, U. (2007). Aerosol partitioning between the interstitial and the condensed phase in mixed‐phase clouds. Journal of Geophysical Research: Atmospheres, 112(D23). https://irf.fhnw.ch/handle/11654/46703