Impact of anthropogenic aerosols on summer precipitation in the Beijing–Tianjin–Hebei urban agglomeration in China: Regional climate modeling using WRF-Chem

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• 作者：Jun Wang ; Jinming Feng ; Qizhong Wu ; Zhongwei Yan
• 关键词：anthropogenic aerosols ; summer precipitation ; urban agglomeration ; regional climate
• 刊名：Advances in Atmospheric Sciences
• 出版年：2016
• 出版时间：June 2016
• 年：2016
• 卷：33
• 期：6
• 页码：753-766
• 全文大小：6,377 KB
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• 作者单位：Jun Wang (1)
  Jinming Feng (1)
  Qizhong Wu (2)
  Zhongwei Yan (1)
  
  1. Key Laboratory of Regional Climate-Environment for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China
  2. College of Global Change and Earth System Science, Beijing Normal University, Beijing, 100875, China
  
• 刊物主题：Atmospheric Sciences; Meteorology; Geophysics/Geodesy;
• 出版者：Springer Berlin Heidelberg
• ISSN：1861-9533

文摘

The WRF model with chemistry (WRF-Chem) was employed to simulate the impacts of anthropogenic aerosols on summer precipitation over the Beijing–Tianjin–Hebei urban agglomeration in China. With the aid of a high-resolution gridded inventory of anthropogenic emissions of trace gases and aerosols, we conducted relatively long-term regional simulations, considering direct, semi-direct and indirect effects of the aerosols. Comparing the results of sensitivity experiments with and without emissions, it was found that anthropogenic aerosols tended to enhance summer precipitation over the metropolitan areas. Domain-averaged rainfall was increased throughout the day, except for the time around noon. Aerosols shifted the precipitation probability distribution from light or moderate to extreme rain. Further analysis showed that the anthropogenic aerosol radiative forcing had a cooling effect at the land surface, but a warming effect in the atmosphere. However, enhanced convective strength and updrafts accompanied by water vapor increases and cyclone-like wind shear anomalies were found in the urban areas. These responses may originate from cloud microphysical effects of aerosols on convection, which were identified as the primary cause for the summer rainfall enhancement.