TY - JOUR
T1 - Aerosol optical properties over urban and industrial region of Northeast China by using ground-based sun-photometer measurement
AU - Zhao, Hujia
AU - Che, Huizheng
AU - Zhang, Xiaoye
AU - Ma, Yanjun
AU - Wang, Yangfeng
AU - Wang, Xuxin
AU - Liu, Chuang
AU - Hou, Bo
AU - Che, Haochi
N1 - Funding Information:
This work is financially supported by grants from the National Key Project of Basic Research ( 2011CB403401 ), the Project ( 41005086 & 41130104 ) supported by NSFC , CAMS Basis Research Project ( 2012Y02 & 2010Z002 ), the Meteorological Special Project of China ( GYHY-200906038 & 201206037 ), and the Project supported by Ministry of Science and Technology of China ( 2010DFA22770 ).
PY - 2013/8
Y1 - 2013/8
N2 - The special and temporal characteristics of aerosol optical depth (AOD) and Angstrom exponent (Alpha) were analyzed by using the data from a CE318 sun-photometer at Shenyang, Anshan, Benxi and Fushun in urban and industrial region of northeastern China. The high AODs over Shenyang and Fushun occurred in the summer and winter with two peaks. In contrast, the monthly averaged AODs at Anshan and Benxi have a single peak distribution. The AOD frequency distribution at Shenyang and Benxi can be well fit by a bi-modal normal distribution with r2=0.94 and 0.91. The AOD frequency distribution at Anshan and Fushun have identical peak value at approximately 0.40. The seasonal AOD at Benxi is larger than the other three stations, and the seasonal Alpha at Shenyang is the largest of all stations followed by Anshan, Fushun and Benxi. An analysis of the AOD and Alpha scatterplots suggests that the aerosol size in Shenyang, Anshan, Benxi and Fushun can be affected by both fine and coarse particles.
AB - The special and temporal characteristics of aerosol optical depth (AOD) and Angstrom exponent (Alpha) were analyzed by using the data from a CE318 sun-photometer at Shenyang, Anshan, Benxi and Fushun in urban and industrial region of northeastern China. The high AODs over Shenyang and Fushun occurred in the summer and winter with two peaks. In contrast, the monthly averaged AODs at Anshan and Benxi have a single peak distribution. The AOD frequency distribution at Shenyang and Benxi can be well fit by a bi-modal normal distribution with r2=0.94 and 0.91. The AOD frequency distribution at Anshan and Fushun have identical peak value at approximately 0.40. The seasonal AOD at Benxi is larger than the other three stations, and the seasonal Alpha at Shenyang is the largest of all stations followed by Anshan, Fushun and Benxi. An analysis of the AOD and Alpha scatterplots suggests that the aerosol size in Shenyang, Anshan, Benxi and Fushun can be affected by both fine and coarse particles.
KW - Aerosol optical depth
KW - Angstrom exponent
KW - Northeast China
KW - Sun-photometer
UR - http://www.scopus.com/inward/record.url?scp=84877912633&partnerID=8YFLogxK
U2 - 10.1016/j.atmosenv.2013.04.048
DO - 10.1016/j.atmosenv.2013.04.048
M3 - ???researchoutput.researchoutputtypes.contributiontojournal.article???
AN - SCOPUS:84877912633
SN - 1352-2310
VL - 75
SP - 270
EP - 278
JO - Atmospheric Environment
JF - Atmospheric Environment
ER -