Characteristics of Turbulence and Aerosol Optical and Radiative Properties during Haze-Fog Episodes in Shenyang, Northeast China

被引:4
作者
Li, Xiaolan [1 ]
Ma, Yanjun [1 ]
Wang, Yangfeng [1 ]
Lu, Shuo [2 ]
Zhao, Hujia [1 ]
Liu, Ningwei [1 ]
Hong, Ye [1 ]
Wang, Dongdong [1 ]
机构
[1] China Meteorol Adm, Inst Atmospher Environm, Shenyang 110166, Peoples R China
[2] Nanjing Univ Informat Sci & Technol, Key Lab Aerosol Cloud Precipitat, China Meteorol Adm, Nanjing 210044, Peoples R China
基金
中国国家自然科学基金;
关键词
haze and fog; turbulence; radiative effect; optical property; planetary boundary layer; Northeast China; PM2.5; VISIBILITY; POLLUTION; EVENTS; WINTER;
D O I
10.3390/atmos12121658
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The characteristics of turbulence in the planetary boundary layer (PBL) and the aerosol optical and radiative properties during haze and haze-fog mixed episodes on 22-27 January 2021, in Shenyang, a provincial city in Northeast China, were analyzed using meteorological and aerosol observations. During the haze episode, the hourly mean PM2.5 concentration reached a maximum of 337 mu g m(-3) and visibility decreased to 1.6 km. The PM2.5 concentration decreased gradually during the haze-fog mixed episode as a result of the scavenging effects of fog, but visibility mostly remained below 1 km owing to high ambient relative humidity (>90%). During the haze-fog mixed episode, an increasing proportion of PM2.5 led to a higher ratio of the backward to the total scattering coefficient. As fog occurred, downward shortwave radiation arriving at the surface was significantly reduced, and upward longwave radiation increased and almost equaled the downward longwave radiation, which can be used as a good indicator for distinguishing haze and fog. Mechanical turbulence was weak during both episodes, and latent heat flux varied within a wider range during the haze-fog mixed episode. The PBL dynamic structure affected the vertical distribution of aerosols/fog droplets. Aerosol-rich layers appeared at altitudes below 0.5 km and above 0.6 km during the haze episode. The elevated aerosol layer was related to the aerosol transport from upstream polluted areas caused by strong upper-level turbulence, and it began to mix vertically after sunrise because of convective turbulence. Aerosols and fog droplets were mostly trapped in a shallower PBL with a height of 0.2-0.4 km during the haze-fog mixed episode because of weaker turbulence.
引用
收藏
页数:15
相关论文
共 39 条
  • [21] Atmospheric boundary layer turbulence structure for severe foggy haze episodes in north China in December 2016
    Li, Xin
    Gao, Chloe Y.
    Gao, Zhiqiu
    Zhang, Xiaoye
    [J]. ENVIRONMENTAL POLLUTION, 2020, 264
  • [22] Characteristics of Aerosol during a Severe Haze-Fog Episode in the Yangtze River Delta: Particle Size Distribution, Chemical Composition, and Optical Properties
    Liu, Ankang
    Wang, Honglei
    Cui, Yi
    Shen, Lijuan
    Yin, Yan
    Wu, Zhijun
    Guo, Song
    Shi, Shuangshuang
    Chen, Kui
    Zhu, Bin
    Wang, Jinhu
    Kong, Xiangchen
    [J]. ATMOSPHERE, 2020, 11 (01)
  • [23] Understanding of Aerosol-Climate Interactions in China: Aerosol Impacts on Solar Radiation, Temperature, Cloud, and Precipitation and Its Changes Under Future Climate and Emission Scenarios
    Liu, Song
    Xing, Jia
    Zhao, Bin
    Wang, Jiandong
    Wang, Shuxiao
    Zhang, Xiaoye
    Ding, Aijun
    [J]. CURRENT POLLUTION REPORTS, 2019, 5 (02) : 36 - 51
  • [24] Air pollution and meteorological conditions significantly contribute to the worsening of allergic conjunctivitis: a regional 20-city, 5-year study in Northeast China
    Lu, Cheng-Wei
    Fu, Jing
    Liu, Xiu-Fen
    Chen, Wei-Wei
    Hao, Ji-Long
    Li, Xiao-Lan
    Pant, Om Prakash
    [J]. LIGHT-SCIENCE & APPLICATIONS, 2021, 10 (01)
  • [25] Quantifying the relationship between PM2.5 concentration, visibility and planetary boundary layer height for long-lasting haze and fog-haze mixed events in Beijing
    Luan, Tian
    Guo, Xueliang
    Guo, Lijun
    Zhang, Tianhang
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2018, 18 (01) : 203 - 225
  • [26] Addressing the issue of fog and haze: A promising perspective from meteorological science and technology
    Mu Mu
    Zhang RenHe
    [J]. SCIENCE CHINA-EARTH SCIENCES, 2014, 57 (01) : 1 - 2
  • [27] Pruppacher H. R., 1978, MICROPHYSICS CLOUDS, P9, DOI DOI 10.1007/978-94-009-9905-3_2
  • [28] Analysis of the formation of fog and haze in North China Plain (NCP)
    Quan, J.
    Zhang, Q.
    He, H.
    Liu, J.
    Huang, M.
    Jin, H.
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2011, 11 (15) : 8205 - 8214
  • [29] Reddy MS, 2000, ATMOS ENVIRON, V34, P4511
  • [30] Particulate air pollution and health inequalities: a Europe-wide ecological analysis
    Richardson, Elizabeth A.
    Pearce, Jamie
    Tunstall, Helena
    Mitchell, Richard
    Shortt, Niamh K.
    [J]. INTERNATIONAL JOURNAL OF HEALTH GEOGRAPHICS, 2013, 12