Carbonaceous aerosols affect the global radiative balance by absorbing and scattering
radiation, which leads to warming or cooling of the atmosphere, respectively. Black carbon is …

Airborne observations over the Amazon Basin showed high aerosol particle concentrations
in the upper troposphere (UT) between 8 and 15 km altitude, with number densities …

Existing studies on vertical profiling of black carbon (BC) and ozone (O 3) were mainly
conducted in the rural areas, leading to limited knowledge of their vertical distributions in the …

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 …

Black Carbon (BC) aerosols substantially affect the global climate. However, accurate
simulation of BC atmospheric transport remains elusive, due to shortcomings in modeling …

The size-resolved properties of atmospheric black carbon (BC) importantly determine its
absorption capacity and cloud condensation nuclei (CCN) ability. This study reports …

The abrupt reduction in human activities during the first lockdown of the COVID-19
pandemic created unprecedented atmospheric conditions. To quantify the changes in lower …

Black carbon (BC) concentrations observed in 22 snowpits sampled in the northwest sector
of the Greenland ice sheet in April 2014 have allowed us to identify a strong and widespread …

Black carbon (BC) aerosols from incomplete combustion generally warm the climate, but the
magnitudes of their various interactions with climate are still uncertain. A key knowledge gap …

We use the Weather Research and Forecasting with Chemistry (WRF-Chem) model with
new implementations of GOES-16 wildfire emissions and plume rise based on fire radiative …