Vertical evolution of black and brown carbon during pollution events over North China Plain

The vertical distribution of carbonaceous aerosol impacts climate change, air quality and human health, but there is a lack of in-situ vertical observations of black (BC) and brown carbon (BrC). Thus, the characteristic of vertical profiles of BC concentration, particle number concentration (PNC), O-3 concentration and optical absorption of BC and BrC were observed in a suburban site over North China Plain. where heavy pollution of PM2.5 and O-3 always occurred in winter and summer, respectively. In winter, during a heavy pollution episode, the BC and PNC was near uniformly distributed within mixing layer (ML) (15.2 +/- 6.7 mu g m(-3) and 678 +/- 227 p cm(-3), respectively) and decreased with altitude above the ML The BC heating rate reached about 0.13 K h(-1) during the heaviest pollution day. In summer, the BC concentration (2.9 +/- 1.3 mu g m(-3)) in ML during the middle O-3 pollution events was higher than that (1.7 +/- 0.6 mu g m(-3)) during the light O-3 pollution. The light absorption coefficients of BC at 880 nm and BrC at 375 nm measured in the early morning were lower than that in the daytime, and the contribution of BrC to total light absorption of carbonaceous aerosols was in the range of 27-47%. In addition, BC was effectively transported to high altitude than BrC in the daytime. The light absorption of secondary BrC in the daytime was higher 10-20% than that in the early morning. Simultaneously, the contribution of secondary BrC to the total BrC light absorption at 375 nm was range from 32% to 68% within 1000 m. (C) 2021 Elsevier B.V. All rights reserved.

Automated summary

The study found that in a suburban site over North China Plain, BC and PNC were nearly uniformly distributed within the mixing layer during winter pollution episodes, while decreasing with altitude above the mixing layer. In summer, the BC concentration was higher during moderate O-3 pollution events, and BrC contributed to 27-47% of the total light absorption of carbonaceous aerosols.