Articles | Volume 15, issue 8
https://doi.org/10.5194/acp-15-4279-2015
https://doi.org/10.5194/acp-15-4279-2015
Research article
 | 
24 Apr 2015
Research article |  | 24 Apr 2015

Modeling the feedback between aerosol and meteorological variables in the atmospheric boundary layer during a severe fog–haze event over the North China Plain

Y. Gao, M. Zhang, Z. Liu, L. Wang, P. Wang, X. Xia, M. Tao, and L. Zhu

Viewed

Total article views: 6,760 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,557 3,075 128 6,760 803 109 164
  • HTML: 3,557
  • PDF: 3,075
  • XML: 128
  • Total: 6,760
  • Supplement: 803
  • BibTeX: 109
  • EndNote: 164
Views and downloads (calculated since 14 Jan 2015)
Cumulative views and downloads (calculated since 14 Jan 2015)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 16 Jul 2024
Download
Short summary
By using an online coupled meteorology and aerosol/chemistry model (WRF-Chem), the increase of surface PM2.5 concentration is estimated to be up to 30% during a severe fog--haze event (10--15 January 2013) over North China Plain owing to the aerosol-induced decreased surface temperature, wind speed and atmosphere boundary layer height, increased surface relative humidity, and more stable atmosphere. A mechanism of positive feedback exists and contributes to the formation of fog--haze events.
Altmetrics
Final-revised paper
Preprint