Atmospheric ice‐nucleating particles (INPs) play a critical role in cloud freezing processes,
with important implications for precipitation formation and cloud radiative properties, and …

Organic matter in the gas‐phase and particles are important components of the atmosphere.
Photochemical degradation is a major transformation pathway of atmospheric organic …

Biomass burning organic aerosol (BBOA) in the atmosphere contains many compounds that
absorb solar radiation, called brown carbon (BrC). While BBOA is in the atmosphere, BrC …

Biomass burning events emit large amounts of phenolic compounds, which are oxidized in
the atmosphere and form secondary organic aerosol (SOA). Using the poke-flow technique …

Biomass burning organic aerosol (BBOA), containing brown carbon chromophores, plays a
critical role in atmospheric chemistry and climate forcing. However, the effects of evaporation …

A sensitive analytical method has been developed and validated for the determination of 16
polyfluorinated alkyl substances (PFAS) in fine airborne particulate matter (PM 2.5) using on …

Aerosol acidity increases secondary organic aerosol (SOA) formed from the reactive uptake
of isoprene-derived epoxydiols (IEPOX) by enhancing condensed-phase reactions within …

Prediction of ice formation in clouds presents one of the grand challenges in the
atmospheric sciences. Immersion freezing initiated by ice-nucleating particles (INPs) is the …

Information on the global distributions of secondary organic aerosol (SOA) phase state and
mixing times within SOA is needed to predict the impact of SOA on air quality, climate, and …

Viscosity is a fundamental physicochemical property of aerosol particles that influences
chemical evolution, mass transfer rates, particle formation, etc. and also changes with …