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

Herbivore induced plant volatiles (HIPVs) are specific volatile organic compounds (VOC)
that a plant produces in response to herbivory. Some HIPVs are only produced after …

Marine low clouds play an important role in the climate system, and their properties are
sensitive to cloud condensation nuclei concentrations. While new particle formation …

The secondary organic aerosol (SOA) mass yields from NO3 oxidation of a series of
biogenic volatile organic compounds (BVOCs), consisting of five monoterpenes and one …

Atmospheric new particle formation significantly affects global climate and air quality after
newly formed particles grow above∼ 50 nm. In polluted urban atmospheres with 1–3 orders …

This paper describes and evaluates a new framework for modeling kinetic gas-particle
partitioning of secondary organic aerosol (SOA) that takes into account diffusion and …

Airborne nanoparticles are receiving growing attention due to their impacts on human
health, air quality, and climate. Additionally, there are increasing applications of aerosol …

How secondary aerosols form is critical as aerosols' impact on Earth's climate is one of the
main sources of uncertainty for understanding global warming. The beginning stages for …

Ultrafine particles (UFPs) dominate the particle number population in the urban atmosphere
and revealing their chemical composition is important. The thermal desorption chemical …

Investigation of the consecutive reactions of first-generation terpene oxidation products
provides insight into the formation of secondary organic aerosol (SOA). To this end, OH …