Anthropogenic emissions and land use changes have modified atmospheric aerosol
concentrations and size distributions over time. Understanding preindustrial conditions and …

The importance of organic aerosol particles in the environment has been long established,
influencing cloud formation and lifetime, absorbing and scattering sunlight, affecting …

Predicting the formation of ice in the atmosphere presents one of the great challenges in
physical sciences with important implications for the chemistry and composition of the …

Atmospheric ice nucleating particles (INPs) influence global climate by altering cloud
formation, lifetime, and precipitation efficiency. The role of secondary organic aerosol (SOA) …

Hygroscopic growth and cloud condensation nuclei activation are key processes for
accurately modeling the climate impacts of organic particulate matter. Nevertheless, the …

Heterogeneous and multiphase reactions of ozone are important pathways for chemical
ageing of atmospheric organic aerosols. To demonstrate and quantify how moisture-induced …

Highly oxygenated organic molecules (HOMs) are formed from the oxidation of biogenic and
anthropogenic gases and affect Earth's climate and air quality by their key role in particle …

Organic aerosol particles are known to often absorb/desorb water continuously with change
in gas phase relative humidity (RH) without crystallization. Indeed, the prevalence of …

To improve predictions of air quality, visibility, and climate change, knowledge of the
viscosities and diffusion rates within organic particulate matter consisting of secondary …

New measurements of water diffusion in secondary organic aerosol (SOA) material
produced by oxidation of α-pinene and in a number of organic/inorganic model mixtures (3 …