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 (
NCCN) to aerosol concentration (
NCN) 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
NCCN ranged from ~500 cm
−3 at SS = 0.15% to ~2100 cm
−3 at SS = 0.70%, and the mean bulk
NCCN /
NCN ratio ranged from 0.16 at SS = 0.15% to 0.65 at SS = 0.70%. The average critical mobility diameters (
D50) 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
CCN) were 0.39, 0.36, 0.31, and 0.28. The decrease in κ
CCN 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
CCN correlates reasonably well with κ
AMS_SR based on size-resolved AMS measurements: κ
AMS_SR = κ
org ×
forg + κ
inorg ×
finorg, where
forg and
finorg are the organic and inorganic volume fractions, respectively, κ
org = 0.1 and κ
inorg = 0.6, with a
R2 of 0.51.
In closure analysis,
NCCN was estimated by integrating the measured size-resolved
NCN for particles larger than
D50 derived from κ assuming internal mixing state. Estimates using κ
AMS_SR show that the measured and predicted
NCCN were generally within 10% of each other at all four SS. The deviation increased to 26% when κ
AMS was calculated from bulk PM
1 AMS measurements of particles because PM
1 was dominated by particles of 200 to 500 nm in diameter, which had a larger inorganic fraction than those of
D50 (particle diameter < 200 nm). A constant κ = 0.33 (the average value of κ
AMS_SR over the course of campaign) was found to give an
NCCN prediction within 12% of the actual measured values. We also compared
NCCN estimates based on the measured average
D50 and the average size-resolved CCN activation ratio to examine the relative importance of hygroscopicity and mixing state.
NCCN 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.
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