Aerosol particles in the atmosphere profoundly influence public health and climate. Ultrafine
particles enter the body through the lungs and can translocate to essentially all organs, and …

New particle formation of liquid or solid nanoparticles from gas-phase precursors is a
decisive process in Earth's atmosphere and is considered one of the largest uncertainties in …

Secondary organic aerosol contributes a significant fraction to aerosol mass and toxicity.
Low-volatility organic vapours are critical intermediates connecting the oxidation of volatile …

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

Organic aerosol (OA) is the largest and most complicated component of aerosols that greatly
affect human health and global climate. However, widely used models cannot reproduce …

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 …

The mechanistic pathway by which high relative humidity (RH) affects gas–particle
partitioning remains poorly understood, although many studies report increased secondary …

Intense and frequent new particle formation (NPF) events have been observed in polluted
urban environments, yet the dominant mechanisms are still under debate. To understand the …

The large concentrations of ultrafine particles consistently observed at high altitudes over
the tropics represent one of the world's largest aerosol reservoirs, which may be providing a …

The interaction between nitrogen monoxide (NO) and organic peroxy radicals (RO2) greatly
impacts the formation of highly oxygenated organic molecules (HOM), the key precursors of …