Organic peroxides (POs) are organic molecules with one or more peroxide (− O–O−)
functional groups. POs are commonly regarded as chemically labile termination products …

Highly oxygenated organic molecules (HOM) are formed in the atmosphere via autoxidation
involving peroxy radicals arising from volatile organic compounds (VOC). HOM condense on …

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

About half of present-day cloud condensation nuclei originate from atmospheric nucleation,
frequently appearing as a burst of new particles near midday. Atmospheric observations …

Atmospheric aerosols and their effect on clouds are thought to be important for
anthropogenic radiative forcing of the climate, yet remain poorly understood. Globally …

Biogenic vapors form new particles in the atmosphere, affecting global climate. The
contributions of monoterpenes and isoprene to new particle formation (NPF) have been …

Oxidation products of monoterpenes and isoprene have a major influence on the global
secondary organic aerosol (SOA) burden and the production of atmospheric nanoparticles …

New particle formation (NPF) is the source of over half of the atmosphere's cloud
condensation nuclei, thus influencing cloud properties and Earth's energy balance. Unlike in …

Much of our understanding of atmospheric secondary organic aerosol (SOA) formation from
volatile organic compounds derives from laboratory chamber measurements, including …

Dimeric accretion products have been observed both in atmospheric aerosol particles and in
the gas phase. With their low volatilities, they are key contributors to the formation of new …