首页|An analysis of air pollution associated with the 2023 sand and dust storms over China:Aerosol properties and PM10 variability
An analysis of air pollution associated with the 2023 sand and dust storms over China:Aerosol properties and PM10 variability
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Every spring,a large part of China is confronted with sand and dust storms(SDS)-mainly originating in the Gobi(including Chinese and Mongolian Gobi)and Taklamakan deserts.In March-April 2023,most of northern,northwestern and northeastern China was struck by three sandstorms that affected an area with more than 500 million people.In this study,aerosol optical,microphysical and radiative properties were studied during these SDS events using an integrated approach that combines satellite,terrestrial and re-analysis data.The results showed that dusty conditions were observed in most areas north of the Yangtze River(ChangJiang)with daily average PM10 concentrations exceeding 1000 pg/m3 in many cities.VIIRS aerosol optical depth(AOD)at 550 nm during three SDS events exceeded a value of 1 throughout nearly the entire northern part of the country.The AERONET data obtained from the AOE_Baotou site showed a significant increase in total AOD and a corresponding decrease in AE during the SDS.The single scattering albedo(SSA),asymmetry parameter(ASY),real refractive index(RRI)and imaginary refractive index(IRI)values indicate an abundance of scattering coarse-mode particles.Aerosol radiative forcing(ARF)at top of the atmosphere and at the earth's surface was nearly always neg-ative during the period and ranged from-48.5 to+2.7 Wm-2 and from-180.8 to-66.6 Wm-2,resulting in high positive ARF values at ATM(from+63.8 to+132.3 Wm-2).Each of these affects the heating of the atmosphere and cooling on the earth's surface.The atmospheric heating rates ranged from 1.8 to 3.7 K day-1.The formation of these SDS mainly resulted from the passage of cold fronts associated with low pressure systems in the Gobi and Taklamakan deserts,creating conditions for dust to rise into the atmosphere and move further downwind.
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