Size-resolved cloud condensation nuclei (CCN) activity and closure analysis at the HKUST Supersite in Hong Kong
The cloud condensation nuclei (CCN) properties of atmospheric aerosols were measured on 1–30 May 2011 at the HKUST (Hong Kong University of Science and Technology) Supersite, a coastal site in Hong Kong. Size-resolved CCN activation curves, the ratio of number concentration of CCN (<i>N</i&...
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doaj-63aa2a8b63764f20b2bc7fef12cd57802020-11-24T22:45:47ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242014-09-011418102671028210.5194/acp-14-10267-2014Size-resolved cloud condensation nuclei (CCN) activity and closure analysis at the HKUST Supersite in Hong KongJ. W. Meng0M. C. Yeung1Y. J. Li2B. Y. L. Lee3C. K. Chan4Division of Environment, The Hong Kong University of Science and Technology, Clear Water Bay, Hong Kong SAR, ChinaDepartment of Chemical and Biomolecular Engineering, The Hong Kong University of Science and Technology, Clear Water Bay, Hong Kong SAR, ChinaDivision of Environment, The Hong Kong University of Science and Technology, Clear Water Bay, Hong Kong SAR, ChinaDivision of Environment, The Hong Kong University of Science and Technology, Clear Water Bay, Hong Kong SAR, ChinaDivision of Environment, The Hong Kong University of Science and Technology, Clear Water Bay, Hong Kong SAR, ChinaThe cloud condensation nuclei (CCN) properties of atmospheric aerosols were measured on 1–30 May 2011 at the HKUST (Hong Kong University of Science and Technology) Supersite, a coastal site in Hong Kong. Size-resolved CCN activation curves, the ratio of number concentration of CCN (<i>N</i><sub>CCN</sub>) to aerosol concentration (<i>N</i><sub>CN</sub>) as a function of particle size, were obtained at supersaturation (SS) = 0.15, 0.35, 0.50, and 0.70% using a DMT (Droplet Measurement Technologies) CCN counter (CCNc) and a TSI scanning mobility particle sizer (SMPS). The mean bulk size-integrated <i>N</i><sub>CCN</sub> ranged from ~500 cm<sup>−3</sup> at SS = 0.15% to ~2100 cm<sup>−3</sup> at SS = 0.70%, and the mean bulk <i>N</i><sub>CCN</sub> / <i>N</i><sub>CN</sub> ratio ranged from 0.16 at SS = 0.15% to 0.65 at SS = 0.70%. The average critical mobility diameters (<i>D</i><sub>50</sub>) at SS = 0.15, 0.35, 0.50, and 0.70% were 116, 67, 56, and 46 nm, respectively. The corresponding average hygroscopic parameters (κ<sub>CCN</sub>) were 0.39, 0.36, 0.31, and 0.28. The decrease in κ<sub>CCN</sub> can be attributed to the increase in organic to inorganic volume ratio as particle size decreases, as measured by an Aerodyne high resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS). The κ<sub>CCN</sub> correlates reasonably well with κ<sub>AMS_SR</sub> based on size-resolved AMS measurements: κ<sub>AMS_SR</sub> = κ<sub>org</sub> × <i>f</i><sub>org</sub> + κ<sub>inorg</sub> × <i>f</i><sub>inorg</sub>, where <i>f</i><sub>org</sub> and <i>f</i><sub>inorg</sub> are the organic and inorganic volume fractions, respectively, κ<sub>org</sub> = 0.1 and κ<sub>inorg</sub> = 0.6, with a <i>R</i><sup>2</sup> of 0.51. <br><br> In closure analysis, <i>N</i></sub>CCN</sub> was estimated by integrating the measured size-resolved <i>N</i></sub>CN</sub> for particles larger than <i>D</i><sub>50</sub> derived from κ assuming internal mixing state. Estimates using κ<sub>AMS_SR</sub> show that the measured and predicted <i>N</i><sub>CCN</sub> were generally within 10% of each other at all four SS. The deviation increased to 26% when κ<sub>AMS</sub> was calculated from bulk PM<sub>1</sub> AMS measurements of particles because PM<sub>1</sub> was dominated by particles of 200 to 500 nm in diameter, which had a larger inorganic fraction than those of <i>D</i><sub>50</sub> (particle diameter < 200 nm). A constant κ = 0.33 (the average value of κ<sub>AMS_SR</sub> over the course of campaign) was found to give an <i>N</i><sub>CCN</sub> prediction within 12% of the actual measured values. We also compared <i>N</i><sub>CCN</sub> estimates based on the measured average <i>D</i><sub>50</sub> and the average size-resolved CCN activation ratio to examine the relative importance of hygroscopicity and mixing state. <i>N</i><sub>CCN</sub> appears to be relatively more sensitive to the mixing state and hygroscopicity at a high SS = 0.70% and a low SS = 0.15%, respectively.http://www.atmos-chem-phys.net/14/10267/2014/acp-14-10267-2014.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
J. W. Meng M. C. Yeung Y. J. Li B. Y. L. Lee C. K. Chan |
spellingShingle |
J. W. Meng M. C. Yeung Y. J. Li B. Y. L. Lee C. K. Chan Size-resolved cloud condensation nuclei (CCN) activity and closure analysis at the HKUST Supersite in Hong Kong Atmospheric Chemistry and Physics |
author_facet |
J. W. Meng M. C. Yeung Y. J. Li B. Y. L. Lee C. K. Chan |
author_sort |
J. W. Meng |
title |
Size-resolved cloud condensation nuclei (CCN) activity and closure analysis at the HKUST Supersite in Hong Kong |
title_short |
Size-resolved cloud condensation nuclei (CCN) activity and closure analysis at the HKUST Supersite in Hong Kong |
title_full |
Size-resolved cloud condensation nuclei (CCN) activity and closure analysis at the HKUST Supersite in Hong Kong |
title_fullStr |
Size-resolved cloud condensation nuclei (CCN) activity and closure analysis at the HKUST Supersite in Hong Kong |
title_full_unstemmed |
Size-resolved cloud condensation nuclei (CCN) activity and closure analysis at the HKUST Supersite in Hong Kong |
title_sort |
size-resolved cloud condensation nuclei (ccn) activity and closure analysis at the hkust supersite in hong kong |
publisher |
Copernicus Publications |
series |
Atmospheric Chemistry and Physics |
issn |
1680-7316 1680-7324 |
publishDate |
2014-09-01 |
description |
The cloud condensation nuclei (CCN) properties of atmospheric aerosols were
measured on 1–30 May 2011 at the HKUST (Hong Kong University of Science and
Technology) Supersite, a coastal site in Hong Kong. Size-resolved CCN
activation curves, the ratio of number concentration of CCN
(<i>N</i><sub>CCN</sub>) to aerosol concentration (<i>N</i><sub>CN</sub>) as a function
of particle size, were obtained at supersaturation (SS) = 0.15, 0.35,
0.50, and 0.70% using a DMT (Droplet Measurement Technologies) CCN counter
(CCNc) and a TSI scanning mobility particle sizer (SMPS). The mean bulk
size-integrated <i>N</i><sub>CCN</sub> ranged from ~500 cm<sup>−3</sup> at
SS = 0.15% to ~2100 cm<sup>−3</sup> at SS = 0.70%, and
the mean bulk <i>N</i><sub>CCN</sub> / <i>N</i><sub>CN</sub> ratio ranged from 0.16
at SS = 0.15% to 0.65 at SS = 0.70%. The average critical
mobility diameters (<i>D</i><sub>50</sub>) at SS = 0.15, 0.35, 0.50, and 0.70%
were 116, 67, 56, and 46 nm, respectively. The corresponding average
hygroscopic parameters (κ<sub>CCN</sub>) were 0.39, 0.36, 0.31, and
0.28. The decrease in κ<sub>CCN</sub> can be attributed to the increase
in organic to inorganic volume ratio as particle size decreases, as measured
by an Aerodyne high resolution time-of-flight aerosol mass spectrometer
(HR-ToF-AMS). The κ<sub>CCN</sub> correlates reasonably well with
κ<sub>AMS_SR</sub> based on size-resolved AMS measurements:
κ<sub>AMS_SR</sub> = κ<sub>org</sub> × <i>f</i><sub>org</sub>
+ κ<sub>inorg</sub> × <i>f</i><sub>inorg</sub>, where
<i>f</i><sub>org</sub> and <i>f</i><sub>inorg</sub> are the organic and inorganic volume
fractions, respectively, κ<sub>org</sub> = 0.1 and
κ<sub>inorg</sub> = 0.6, with a <i>R</i><sup>2</sup> of 0.51.
<br><br>
In closure analysis, <i>N</i></sub>CCN</sub> was estimated by integrating the
measured size-resolved <i>N</i></sub>CN</sub> for particles larger than <i>D</i><sub>50</sub>
derived from κ assuming internal mixing state. Estimates using
κ<sub>AMS_SR</sub> show that the measured and predicted
<i>N</i><sub>CCN</sub> were generally within 10% of each other at all four SS.
The deviation increased to 26% when κ<sub>AMS</sub> was calculated
from bulk PM<sub>1</sub> AMS measurements of particles because PM<sub>1</sub> was dominated
by particles of 200 to 500 nm in diameter, which had a larger inorganic
fraction than those of <i>D</i><sub>50</sub> (particle diameter < 200 nm). A
constant κ = 0.33 (the average value of κ<sub>AMS_SR</sub>
over the course of campaign) was found to give an <i>N</i><sub>CCN</sub> prediction
within 12% of the actual measured values. We also compared
<i>N</i><sub>CCN</sub> estimates based on the measured average <i>D</i><sub>50</sub> and the
average size-resolved CCN activation ratio to examine the relative importance
of hygroscopicity and mixing state. <i>N</i><sub>CCN</sub> appears to be relatively
more sensitive to the mixing state and hygroscopicity at a high
SS = 0.70% and a low SS = 0.15%, respectively. |
url |
http://www.atmos-chem-phys.net/14/10267/2014/acp-14-10267-2014.pdf |
work_keys_str_mv |
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