Air quality in Beijing has been improved
significantly in recent
years; however, our knowledge of the vertically resolved aerosol chemistry
in summer remains poor. Here, we carried out comprehensive measurements
of aerosol composition, gaseous species, and aerosol optical properties
on a meteorological tower in Beijing in summer and compared with those
measured in winter. Our results showed that aerosol liquid water (ALW)
contributing approximately 50% of the total mass with higher values
aloft played a crucial role in aerosol formation. Particularly, the
higher nitrate concentration in city aloft than at the ground level
during daytime was mainly due to the enhanced gas–particle
partitioning driven by ALW and particle acidity. The vertical profiles
of organic aerosol (OA) factors varied more differently in the urban
boundary layer. Although the ubiquitous decreases in primary OA with
the increase in height were mainly due to the influences of local
emissions and vertical convection, the vertical differences in oxygenated
OA between summer and winter may be related to the photochemical processing
of different biogenic and anthropogenic volatile organic compounds.
The single-scattering albedo, brown carbon, and absorption Ångstrom
exponent of aerosol particles also presented different vertical profiles
between day and night due to the vertical changes in aerosol chemistry.