Optical and hygroscopic properties of black carbon influenced by particle microphysics at the top of the anthropogenically polluted boundary layer

• Main Authors: S. Ding, D. Liu, K. Hu, D. Zhao, P. Tian, F. Wang, R. Li, Y. Chen, H. He, M. Huang, D. Ding
• Format: Article
• Language: English
• Published: Copernicus Publications 2021-01-01
• Series: Atmospheric Chemistry and Physics
• Online Access: https://acp.copernicus.org/articles/21/681/2021/acp-21-681-2021.pdf

<p>Aerosols at the top of the planetary boundary layer (PBL) could modify its atmospheric dynamics by redistributing the solar radiation and start to be activated to form low-level cloud at this layer. Black carbon (BC), as an aerosol component efficiently absorbing solar radiation, can introduce heating and positive radiative effects at this sensitive layer, especially in the polluted PBL over the continent. This study presents continuous measurements of detailed BC properties at a mountain site located at the top of the polluted PBL over the North China Plain, during seasons (3 and 4 weeks of data during winter and summer, respectively) with contrasting emission structure and meteorology. The pollution level was persistently influenced by local surface anthropogenic emission on a daily basis through daytime convective mixing, but the concentration was also enhanced or diluted depending on air mass direction, defined as a neutral, polluted and diluted PBL, respectively. Winter was observed to have a higher BC mass fraction (4 %–8 %) than summer (2 %–7 %). By resolving the detailed particle size-resolved mixing state of BC in optical and hygroscopic models, we found an enhanced BC mass absorption cross section (MAC<span class="inline-formula">_BC</span>) for the polluted PBL (up to 13 <span class="inline-formula">m² g⁻¹</span> at <span class="inline-formula"><i>λ</i></span> <span class="inline-formula">=</span> 550 <span class="inline-formula">nm</span>), which was 5 % higher during summer than winter due to a smaller BC core size. The higher BC mass fraction in winter corresponded to a lower single-scattering albedo by 0.03–0.09 than summer, especially the lowest for the diluted winter PBL (0.86 <span class="inline-formula">±</span> 0.02). The water supersaturation (SS) required to activate half the number of BC decreased from 0.21 % <span class="inline-formula">±</span> 0.08 % to 0.1 % <span class="inline-formula">±</span> 0.03 % for the winter diluted and polluted PBL and from 0.22 % <span class="inline-formula">±</span> 0.06 % to 0.17 % <span class="inline-formula">±</span> 0.05 % for summer. Notably, at the top of the anthropogenically polluted PBL in both seasons, the enlarged BC with enhanced absorption capacity could also be efficiently droplet activated; e.g. winter (summer) BC with an MAC of 9.84 <span class="inline-formula">±</span> 1.2 (10.7 <span class="inline-formula">±</span> 1) <span class="inline-formula">m² g⁻¹</span> could be half activated at SS <span class="inline-formula">=</span> 0.13 % <span class="inline-formula">±</span> 0.06 % (0.18 % <span class="inline-formula">±</span> 0.05 %). This BC at the top of the PBL can more directly interact with the free troposphere and be transported to a wider region, exerting important direct and indirect radiative impacts.</p>