Black carbon (BC) aerosol is of great importance not only for its strong potential in heating
air and impacts on cloud, but also because of its hazards to human health. Wet deposition is …

Cloud droplet number concentration (Nd) is a key microphysical property that is largely
controlled by the balance between sources and sinks of aerosols that serve as cloud …

Current models estimate global aviation contributes approximately 5% to the total
anthropogenic climate forcing, with aerosol‐cloud interactions having the greatest effect …

In‐cloud wet scavenging dominates the wet removal of aerosols in the atmosphere, but is
not well represented in climate models. Aircraft measurements of black carbon (BC) …

This study analyzes long-range transport of aerosol and aerosol chemical characteristics
based on instances of high-and low-aerosol-loading events determined via ground-based …

In the second of two companion papers, we quantify the potential ultimate benefits for public
health and radiative forcing from the phase-out of coal use in China. With the baseline year …

Limited by the scarcity of in situ vertical observation data, the influences of biomass burning
in Southeast Asia on major atmospheric carbonaceous compositions in downwind regions …

Understanding the global distribution of atmospheric black carbon (BC) is essential for
unveiling its climatic effect. However, there are still large uncertainties regarding the …

Soot particles may undergo cloud‐processing during atmospheric transport after which the
particle porosity and surface wettability can be modified. Soot particles therefore show …

Interactions between clouds and black carbon (BC) represent a significant uncertainty in
aerosol radiative forcing. To investigate the influence of cloud processing on the scavenging …