Cheng Yingfei, Zhu Bin, Wang Lijuan, Lu Wen, Kang Hanqing, Gao Jinhui
Key Laboratory of Meteorological Disaster, Ministry of Education (KLME), Joint International Research Laboratory of Climate and Environment Change (ILCEC), Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disaster, Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science and Technology, Nanjing 210044, China.
Key Laboratory of Meteorological Disaster, Ministry of Education (KLME), Joint International Research Laboratory of Climate and Environment Change (ILCEC), Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disaster, Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science and Technology, Nanjing 210044, China.
Sci Total Environ. 2022 Sep 20;840:156517. doi: 10.1016/j.scitotenv.2022.156517. Epub 2022 Jun 6.
Long-range transport (LRT) and local accumulation (LA) are key atmospheric physical processes affecting air pollution formation, and their impacts on surface air pollution have been extensively researched. Due to the lack of vertical observations and emphases on model simulations, the characteristics and regional sources of black carbon (BC) aerosol profiles have been relatively understudied. In this study, the chemistry-coupled Weather Research and Forecasting model (WRF-Chem) with a BC source-tagging method was used to quantify BC source contributions (considering 18 geographical regions over east Asia, including 3 subregions over the Yangtze River Delta (YRD)) during a November 2017 pollution event in the YRD, China. In this event, the YRD mainly experienced a uniform pressure field, stable weather and weak wind fields. During the uniform high-pressure period, the dominant contribution to surface BC in each sub-region was from that region itself (70.6 %-98.2 %), with little intra- and inter-regional transport. During the uniform low-pressure period, highly variable contributions to the surface BC from intra-regional transport within the YRD (0.05 %-65.9 %) and inter-regional transport outside the YRD (mostly from Anhui (AH) to the west of the YRD, 0.37 %-23.9 %) were simulated. In the vertical direction, the dominant contributors were local YRD sources (73.8 %-94.2 %) below the atmospheric boundary layer (ABL). The inter-transport contributions increased extensively above the ABL. As a westerly trough crossing, a long-range inter-regional transport from South China (SCHN, 3.3 %) and the North China Plain (NCP, 2.7 %) was simulated above the ABL. We found that when the surface experienced similar stable weather conditions, the weather conditions in the upper air may have been quite different, resulting in significant differences in the regional transport of BC in the upper ABL. This study provides a reference for improving air quality from the local scale to the regional scale.
长距离传输(LRT)和局地积累(LA)是影响空气污染形成的关键大气物理过程,它们对地表空气污染的影响已得到广泛研究。由于缺乏垂直观测以及对模型模拟的重视,黑碳(BC)气溶胶廓线的特征和区域来源相对研究较少。在本研究中,利用带有BC源标记方法的化学耦合气象研究与预报模型(WRF-Chem),对2017年11月中国长江三角洲(YRD)污染事件期间的BC源贡献进行了量化(考虑东亚的18个地理区域,包括长江三角洲的3个次区域)。在该事件中,长江三角洲主要经历了均匀的压力场、稳定的天气和弱风场。在均匀高压期,每个次区域地表BC的主要贡献来自该区域本身(70.6%-98.2%),区域内和区域间传输较少。在均匀低压期,模拟了长江三角洲区域内传输(0.05%-65.9%)和长江三角洲区域外区域间传输(主要从安徽(AH)到长江三角洲西部,0.37%-23.9%)对地表BC的高度可变贡献。在垂直方向上,大气边界层(ABL)以下的主要贡献者是长江三角洲本地源(73.8%-94.2%)。ABL以上区域间传输贡献大幅增加。作为一个西风槽过境,在ABL以上模拟了来自中国南方(SCHN,3.3%)和华北平原(NCP,2.7%)的长距离区域间传输。我们发现,当地表经历相似的稳定天气条件时,高空的天气条件可能有很大不同,导致ABL上部BC的区域传输存在显著差异。本研究为从局部尺度到区域尺度改善空气质量提供了参考。