Causes of an extremely low visibility event in Northeast China

An extreme haze‐fog event occurred during October 20–22, 2013, in Harbin, Northeast China, which lasted for nearly 60 h with local visibility as low as 20 m. However, causes of the extreme haze‐fog formation remain unclear. Through the analysis of in situ data and objective weather circulation class...

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Veröffentlicht in:Meteorological applications 2024-03, Vol.31 (2), p.n/a
Hauptverfasser: Cao, Dianbin, Chen, Xuelong, Zhang, Qiang, Lin, Yanluan, Zhang, Qinghong, Ma, Yaoming
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Sprache:eng
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Zusammenfassung:An extreme haze‐fog event occurred during October 20–22, 2013, in Harbin, Northeast China, which lasted for nearly 60 h with local visibility as low as 20 m. However, causes of the extreme haze‐fog formation remain unclear. Through the analysis of in situ data and objective weather circulation classification, it is revealed that high pollutant emissions from biomass burning played a very important role in the extreme event. Stable weather conditions under the circulation type 8 (CT8), marked by weak high‐pressure control, strong inversion (6.55°C), shallow boundary layer depth (90%), aided in the accumulation of pollutants and hygroscopic aerosol growth. All of these factors collectively contributed to the extreme haze‐fog formation. The insights derived from this study can improve the predictability of extreme haze‐fog events, and indicate that pollution emissions should be tightly controlled in the adverse meteorological circulation type in Northeast China. An extreme haze‐fog event occurred in Harbin, Northeast China, during October 20–22, 2013. It lasted nearly 60 h with local visibility as low as 20 m. Strong inversion (6.55°C), shallow boundary layer (90%), and high pollutant emissions from biomass burning collectively contributed to the extreme haze‐fog formation. The insights derived from this study can improve the predictability of extreme haze‐fog events, and indicate that pollution emissions should be tightly controlled in the adverse meteorological circulation type in Northeast China.
ISSN:1350-4827
1469-8080
DOI:10.1002/met.2199