资源环境科技发展态势分析平台

Aerosol optical properties were measured in Beijing in summer and winter using a state-of-the-art cavity attenuated phase shift single scattering albedo monitor (CAPS PMssa) along with aerosol composition measurements by aerosol mass spectrometers and aethalometers. The SSA directly measured by the CAPS PMssa showed overall agreements with those derived from colocated measurements. However, substantial differences were observed during periods with low SSA values in both summer and winter, suggesting that interpretation of low SSA values needs to be cautious. The average (+/-sigma) extinction coefficient (b(ext)) and absorption coefficient (b(ap)) were 336 (+/- 343) Mm(-1) and 44 (+/- 41) Mm(-1), respectively, during wintertime, which were approximately twice those observed in summer, while the average SSA was relatively similar, 0.86 (+/- 0.06) and 0.85 (+/- 0.04) in summer and winter, respectively. Further analysis showed that the variations in SSA can be approximately parameterized as a function of mass fraction of secondary particulate matter (f(SPM)), which is SSA = 0.74 + 0.19 x f(SPM) (f(SPM) > 0.3, r(2) = 0.85). The contributions of aerosol species to extinction coefficients during the two seasons were also estimated. Our results showed that the light extinction was dominantly contributed by ammonium sulfate (30%) and secondary organic aerosol (22%) in summer, while organic aerosol was the largest contributor (51%) in winter. Consistently, SPM played the major role in visibility degradation in both seasons by contributing 70% of the total extinction.