摘要
In order to understand the seasonal variation of aerosol optical properties in the Yangtze River Delta,5 years of measurements were conducted during September 2005 to December 2009 at Taihu,China.The monthly averages of aerosol optical depth were commonly 0.6;the maximum seasonal average（0.93） occurred in summer.The magnitude of the Angstr¨om exponent was found to be high throughout the year;the highest values occurred in autumn（1.33） and were the lowest in spring（1.08）.The fine modes of volume size distribution showed the maxima（peaks） at a radius of ～0.15 μm in spring,autumn,and winter;at a radius of ～0.22 μm in summer.The coarse modes showed the maxima（peaks） at a radius of 2.9 μm in spring,summer,and autumn and at a radius of 3.8 μm in winter.The averages of single-scattering albedo were 0.92（spring）,0.92（summer）,0.91（autumn）,and 0.88（winter）.The averages of asymmetry factor were found to be larger in summer than during other seasons;they were taken as 0.66 at 440-1020 nm over Taihu.The real part of the refractive index showed a weak seasonal variation,with averages of 1.48（spring）,1.43（summer）,1.45（autumn）,and 1.48（winter）.The imaginary parts of the refractive index were higher in winter（0.013） than in spring（0.0076）,summer（0.0092）,and autumn（0.0091）,indicating that the atmosphere in the winter had higher absorbtivity.
In order to understand the seasonal variation of aerosol optical properties in the Yangtze River Delta,5 years of measurements were conducted during September 2005 to December 2009 at Taihu,China.The monthly averages of aerosol optical depth were commonly 0.6;the maximum seasonal average（0.93） occurred in summer.The magnitude of the Angstr¨om exponent was found to be high throughout the year;the highest values occurred in autumn（1.33） and were the lowest in spring（1.08）.The fine modes of volume size distribution showed the maxima（peaks） at a radius of ～0.15 μm in spring,autumn,and winter;at a radius of ～0.22 μm in summer.The coarse modes showed the maxima（peaks） at a radius of 2.9 μm in spring,summer,and autumn and at a radius of 3.8 μm in winter.The averages of single-scattering albedo were 0.92（spring）,0.92（summer）,0.91（autumn）,and 0.88（winter）.The averages of asymmetry factor were found to be larger in summer than during other seasons;they were taken as 0.66 at 440-1020 nm over Taihu.The real part of the refractive index showed a weak seasonal variation,with averages of 1.48（spring）,1.43（summer）,1.45（autumn）,and 1.48（winter）.The imaginary parts of the refractive index were higher in winter（0.013） than in spring（0.0076）,summer（0.0092）,and autumn（0.0091）,indicating that the atmosphere in the winter had higher absorbtivity.
基金
supported by a grant from the National Basic Research Program of China (also called 973 Program,Grant No.2009CB426313)
National Natural Science Foundation of China (Grant Nos. 41005089,41030962 and 40875015)
the Specialized Research Fund for the Doctoral Program of Higher Education of China (Grant No. 20103228120004)
the Natural Science Foundation of the Jiangsu Higher Education Institutions of China (Nos. 08KJA170002 and 10KJB170009),a project funded by the Priority Academic Program Development of Jiangsu Higher Education Institutions
