TY - JOUR
T1 - Size-resolved measurements of mixing state and cloud-nucleating ability of aerosols in Nanjing, China
AU - Ma, Yan
AU - Li, Shizheng
AU - Zheng, Jun
AU - Khalizov, Alexei
AU - Wang, Xing
AU - Wang, Zhen
AU - Zhou, Yaoyao
N1 - Funding Information:
This work is supported by the National Key Research and Development Project 1287 (2016YFC0202401 and 2016YFC0202402), National Natural Science Foundation of China (21377059, 41575122, 41675126, and 91644213), and the Priority Academic Program Development of Jiangsu Higher Education Institutions. A.K. acknowl edges the funding from the National Science Foundation (AGS 1463702). The back trajectories were calculated using the NOAA ARL HYSPLIT model 4.0 (http://ready.arl.noaa.gov/HYSPLIT. php). The fire map was obtained using NASA FIRMS Web Fire Mapper (https:// firms.modaps.eosdis.nasa.gov/firemap/). The other data used are listed in the tables, references, and supporting materials.
PY - 2017/9/16
Y1 - 2017/9/16
N2 - An integrated aerosol analytical system was deployed in Nanjing, a megacity in the Yangtze River Delta, to measure size-resolved aerosol mixing states, effective densities, cloud condensation nucleus (CCN) activities, and chemical composition in August 2013. It was found that aerosols were predominantly internally mixed. The average effective densities were 1.38 ± 0.09, 1.48 ± 0.08, and 1.53 ± 0.07 g cm−3 for 50, 80, and 120 nm particles, respectively. Although black carbon (BC) represented only 0.3%, 1.6%, and 3.3% of the particle mass, on average, it was present in 7%, 38%, and 47% of the total particle number concentration at 50, 80, and 120 nm, respectively, indicating that BC particles may contribute significantly to the total atmospheric aerosol population. Externally mixed BC was only occasionally observed with an effective density of 0.67–0.97 g cm−3. Aerosols sampled generally exhibited a relatively high CCN activity and hygroscopicity (κ = 0.35 ± 0.13). Both newly formed particles and freshly emitted BC particles were observed to age rapidly from photochemical processes, with a significant enhancement in the particle CCN activity and an increase in the effective density. Aerosols influenced by four different air masses presented similar CCN activation, indicating that CCN activation would be primarily dependent on the particle size rather than the particle origin (and hence original composition). Our results suggest that under highly active photochemical conditions as encountered in this study, particles from both local sources and regional transport can be rapidly converted into efficient CCN by photochemical aging, thereby making important contributions to the atmospheric CCN budget and exerting profound implications on aerosol indirect climate forcing.
AB - An integrated aerosol analytical system was deployed in Nanjing, a megacity in the Yangtze River Delta, to measure size-resolved aerosol mixing states, effective densities, cloud condensation nucleus (CCN) activities, and chemical composition in August 2013. It was found that aerosols were predominantly internally mixed. The average effective densities were 1.38 ± 0.09, 1.48 ± 0.08, and 1.53 ± 0.07 g cm−3 for 50, 80, and 120 nm particles, respectively. Although black carbon (BC) represented only 0.3%, 1.6%, and 3.3% of the particle mass, on average, it was present in 7%, 38%, and 47% of the total particle number concentration at 50, 80, and 120 nm, respectively, indicating that BC particles may contribute significantly to the total atmospheric aerosol population. Externally mixed BC was only occasionally observed with an effective density of 0.67–0.97 g cm−3. Aerosols sampled generally exhibited a relatively high CCN activity and hygroscopicity (κ = 0.35 ± 0.13). Both newly formed particles and freshly emitted BC particles were observed to age rapidly from photochemical processes, with a significant enhancement in the particle CCN activity and an increase in the effective density. Aerosols influenced by four different air masses presented similar CCN activation, indicating that CCN activation would be primarily dependent on the particle size rather than the particle origin (and hence original composition). Our results suggest that under highly active photochemical conditions as encountered in this study, particles from both local sources and regional transport can be rapidly converted into efficient CCN by photochemical aging, thereby making important contributions to the atmospheric CCN budget and exerting profound implications on aerosol indirect climate forcing.
KW - Yangtze River Delta
KW - aerosol
KW - black carbon
KW - cloud condensation nuclei
KW - effective density
KW - mixing state
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U2 - 10.1002/2017JD026583
DO - 10.1002/2017JD026583
M3 - Article
AN - SCOPUS:85029215501
SN - 2169-897X
VL - 122
SP - 9430
EP - 9450
JO - Journal of Geophysical Research: Atmospheres
JF - Journal of Geophysical Research: Atmospheres
IS - 17
ER -