The contribution of brown carbon
aerosol to climate forcing remains
poorly understood. Atmospheric processes, such as photochemical aging
and evaporation of brown carbon aerosol, can result in a change in
their physicochemical properties; previous studies have focused on
the effects of such processes in the bulk phase rather than in individual
aerosol particles. We measured direct ultraviolet–visible absorbance
measurements of acoustically levitated aqueous brown carbon droplets.
These show a reproducible red shift in the absorbance maximum as the
droplets evaporate under illumination. This shift does not occur in
the bulk phase. The findings illustrate that common atmospheric processes,
such as evaporation and photochemical aging of brown carbon aerosol,
can cause a red shift in absorbance, leading to a greater overlap
with the solar spectrum. This has implications for the contribution
of brown carbon to radiative forcing of the climate.