This Review aims to summarize the current understanding of bulk tropospheric aqueous-
phase chemistry. Because a complete review of all developments in this area would be …

The acidity of aqueous atmospheric solutions is a key parameter driving both the partitioning
of semi-volatile acidic and basic trace gases and their aqueous-phase chemistry. In addition …

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

The Earth's atmosphere offers a striking contrast with other known planets by its rich organic
composition, which results almost exclusively from the presence of life on the planet. About …

Particles formed in the atmosphere via nucleation provide about half the number of
atmospheric cloud condensation nuclei, but in many locations, this process is limited by the …

Earth's atmosphere contains a multitude of organic compounds, which differ by orders of
magnitude regarding fundamental properties such as volatility, reactivity, and propensity to …

Aerosol particles are important for our global climate, but the mechanisms and especially the
relative importance of various vapors for new particles formation (NPF) remain uncertain …

Secondary organic aerosol (SOA) is ubiquitous in the atmosphere and plays a pivotal role in
climate, air quality, and health. The production of low-volatility dimeric compounds through …

The formation of secondary organic aerosol (SOA) from both ozonolysis and hydroxyl radical
(OH)-initiated oxidation of α-pinene under conditions of high nitric oxide (NO) concentrations …

This study investigates the contribution of high-molecular weight dimer esters to laboratory-
generated α-pinene gas-and particle-phase secondary organic aerosol (SOA) and …