Atmospheric soot and organic particles from fossil fuel combustion and biomass burning
modify Earth's climate through their interactions with solar radiation and through …

Light-absorbing aerosols affect atmospheric radiation, dynamics, and precipitations through
shortwave absorption in the atmosphere and snowpack. Black carbon (BC) is considered …

Clouds play a critical role in modulating the Earth's radiation balance and climate.
Anthropogenic aerosol particles that undergo aging processes, such as soot, aid cloud …

Black carbon (BC) absorbs solar radiation, leading to a strong but uncertain warming effect
on climate. A key challenge in modeling and quantifying BC's radiative effect on climate is …

Soot aggregates form as open, fractal-like structures, but aged atmospheric particles are
often observed to be restructured into more-compact shapes due to internal mixing …

Soot particles are generally considered to be poor ice nucleating particles. Involvement of
soot in clouds and their release back into the atmosphere can form residual particles with …

Atmospheric ice formation in cirrus clouds is often initiated by aerosol particles that act as ice-
nucleating particles. The aerosol–cloud interactions of soot and associated feedbacks …

Biomass burning (BB) fractions estimated with the aethalometer model differ from 0 even for
pure aerosols from fossil fuel (FF) combustion. We used black carbon (BC) aerosols partially …

The convection–cloud chamber enables measurement of aerosol and cloud microphysics,
as well as their interactions, within a turbulent environment under steady‐state conditions …

Stratospheric injections of carbonaceous aerosols and combustion gases by extreme
wildfires have become increasingly common. Recent “megafires,” particularly large and …