Terrestrial vegetation is a major global source of atmospheric secondary organic aerosol
(SOA) through oxidation of biogenic volatile organic compound (BVOC) emissions. Climate …

One barrier to predicting biogenic secondary organic aerosol (SOA) formation in a changing
climate can be attributed to the complex nature of plant volatile emissions. Plant volatile …

The largest global source of secondary organic aerosol (SOA) in the atmosphere is derived
from the oxidation of biogenic emissions. Plant stressors associated with a changing …

Secondary organic aerosol (SOA) impact climate by scattering and absorbing radiation and
contributing to cloud formation. SOA models are based on studies of simplified chemical …

One major challenge in predicting secondary organic aerosol (SOA) formation in the
atmosphere is incomplete representation of biogenic volatile organic compounds (BVOCs) …

Emissions from natural sources are driven by various external stimuli such as sunlight,
temperature, and soil moisture. Once biogenic volatile organic compounds (BVOCs) are …

Emissions of volatile organic compounds (VOC) from vegetation are believed to be a major
source of secondary organic aerosol (SOA), which in turn comprises a large fraction of fine …

Despite the significant contribution of biogenic volatile organic compounds (BVOCs) to
organic aerosol formation and ozone production and loss, there are few long-term, year …

The concentrations of terpenoids (isoprene; monoterpenes, MTs; and sesquiterpenes,
SQTs) and oxygenated volatile organic compounds (OVOCs; ie aldehydes, alcohols …

Emissions of biogenic volatile organic compounds (BVOCs) are important precursors to both
ozone and secondary organic aerosol formation. In this study, we identify and quantify …