Biogenic vapors form new particles in the atmosphere, affecting global climate. The contributions of monoterpenes and isoprene to new particle formation (NPF) have been extensively studied. However, sesquiterpenes have received little attention despite a potentially important role due to their high molecular weight. Via chamber experiments performed under atmospheric conditions, we report biogenic NPF resulting from the oxidation of pure mixtures of β-caryophyllene, α-pinene, and isoprene, which produces oxygenated compounds over a wide range of volatilities. We find that a class of vapors termed ultralow-volatility organic compounds (ULVOCs) are highly efficient nucleators and quantitatively determine NPF efficiency. When compared with a m...
Secondary organic aerosol (SOA), formed by oxidation of volatile organic compounds, substantially in...
Atmospheric oxidation of biogenic hydrocarbons, such as monoterpenes, is estimated to be a significa...
New particle formation (NPF) is an important atmospheric phenomenon. During an NPF event, particles ...
Biogenic vapors form new particles in the atmosphere, affecting global climate. The contributions of...
Oxidation products of monoterpenes and isoprene have a major influence on the global secondary organ...
Nucleation of atmospheric vapours produces more than half of global cloud condensation nuclei and so...
Secondary aerosols formed from anthropogenic pollutants and natural emissions have substantial impac...
Secondary aerosols formed from anthropogenic pollutants and natural emissions have substantial impac...
Secondary organic aerosols (SOAs) formed from biogenic volatile organic compounds (BVOCs) constitute...
Secondary organic aerosol contributes to the atmospheric particle burden with implications for air q...
Atmospheric aerosols are solid or liquid particles suspended in the atmosphere and are either direct...
In the middle of the past century, during the industrial revolution, the concentration of air pollut...
Secondary organic aerosol (SOA) is an important constituent of the atmosphere where SOA particles ar...
Monoterpenes, which are emitted from biogenic and pyrogenic sources, represent a significant mass fr...
Secondary organic aerosol (SOA), formed by oxidation of volatile organic compounds, substantially in...
Atmospheric oxidation of biogenic hydrocarbons, such as monoterpenes, is estimated to be a significa...
New particle formation (NPF) is an important atmospheric phenomenon. During an NPF event, particles ...
Biogenic vapors form new particles in the atmosphere, affecting global climate. The contributions of...
Oxidation products of monoterpenes and isoprene have a major influence on the global secondary organ...
Nucleation of atmospheric vapours produces more than half of global cloud condensation nuclei and so...
Secondary aerosols formed from anthropogenic pollutants and natural emissions have substantial impac...
Secondary aerosols formed from anthropogenic pollutants and natural emissions have substantial impac...
Secondary organic aerosols (SOAs) formed from biogenic volatile organic compounds (BVOCs) constitute...
Secondary organic aerosol contributes to the atmospheric particle burden with implications for air q...
Atmospheric aerosols are solid or liquid particles suspended in the atmosphere and are either direct...
In the middle of the past century, during the industrial revolution, the concentration of air pollut...
Secondary organic aerosol (SOA) is an important constituent of the atmosphere where SOA particles ar...
Monoterpenes, which are emitted from biogenic and pyrogenic sources, represent a significant mass fr...
Secondary organic aerosol (SOA), formed by oxidation of volatile organic compounds, substantially in...
Atmospheric oxidation of biogenic hydrocarbons, such as monoterpenes, is estimated to be a significa...
New particle formation (NPF) is an important atmospheric phenomenon. During an NPF event, particles ...