1.5, aerosol absorption increased, AAE (Absorption Angstrom Exponent) >1.3, and the volume concentration of fine mode particles increased. The peak radius of fine mode particles decreased. The aerosol direct radiation forcing shows that aerosol effect of cooling the top of the atmosphere and the surface at Lhasa and QOMS_CAS stations strengthened, and the effect of heating the atmosphere also strengthened. The possible sources of smoke aerosol were the transportation of biomass burning from Northeast India, Nepal and Bhutan in South Asia."/>
Archive > Volume 50 Issue 6 > 2022,50(6):878-884. DOI:10.19517/j.1671-6345.20210519 Prev Next

Influence of a Biomass Burning Transport Process on Aerosol Optical and Radiation Properties over Tibet Plateau

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