The Earth's atmosphere contains ultrafine particles known as aerosols, which can be either
liquid or solid particles suspended in gas. These aerosols originate from both natural …

Although the particle phase state is an important property, there is scant information on it,
especially, for real-world aerosols. To explore the phase state of fine mode aerosols (PM2 …

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 …

Interactions between atmospheric aerosols, clouds, and precipitation impact Earth's
radiative balance and air quality, yet remain poorly constrained. Precipitating clouds serve …

Recent studies have shown that instantaneous gas-particle equilibrium partitioning
assumptions fail to predict SOA formation, even at high relative humidity (∼ 85%), and …

Water vapor condensation on hygroscopic aerosol particles plays an important role in cloud
formation, climate change, secondary aerosol formation, and aerosol aging. Conventional …

Airborne measurements of non‐refractory bulk aerosol chemical composition, aerosol size
distributions, and cloud condensation nuclei (CCN) were conducted onboard a research …

Evidence has accumulated that secondary organic aerosols (SOAs) exhibit complex
morphologies with multiple phases that can adopt amorphous semisolid or glassy phase …

Elucidating the effects of anthropogenic pollutants on the photooxidation of biogenic volatile
organic compounds is crucial to understanding the fundamental mechanisms of secondary …

A key challenge in aerosol pollution studies and climate change assessment is to
understand how atmospheric aerosol particles are initially formed,. Although new particle …