Area of research
Atmospheric Science · Health, Toxicology and Mutagenesis
Research interest
Research interests include Atmospheric chemistry and aerosols, Atmospheric Ozone and Climate, Air Quality and Health Impacts, and Air Quality Monitoring and Forecasting.
Anthropogenic organic aerosol in Europe produced mainly through second-generation oxidation
Iodine oxoacids enhance nucleation of sulfuric acid particles in the atmosphere
Selective deuteration as a tool for resolving autoxidation mechanisms in <i>α</i> -pinene ozonolysis
High Gas-Phase Methanesulfonic Acid Production in the OH-Initiated Oxidation of Dimethyl Sulfide at Low Temperatures
The gas-phase formation mechanism of iodic acid as an atmospheric aerosol source
Role of iodine oxoacids in atmospheric aerosol nucleation
The driving factors of new particle formation and growth in the polluted boundary layer
Structures and reactivity of peroxy radicals and dimeric products revealed by online tandem mass spectrometry
Rapid growth of new atmospheric particles by nitric acid and ammonia condensation
Multi-generation OH oxidation as a source for highly oxygenated organic molecules from aromatics
Molecular understanding of new-particle formation from <i>α</i> -pinene between −50 and +25 °C
Photo-oxidation of Aromatic Hydrocarbons Produces Low-Volatility Organic Compounds
Enhanced growth rate of atmospheric particles from sulfuric acid
Size-dependent influence of NO <sub>x</sub> on the growth rates of organic aerosol particles
Molecular understanding of the suppression of new-particle formation by isoprene
Unprecedented Ambient Sulfur Trioxide (SO<sub>3</sub>) Detection: Possible Formation Mechanism and Atmospheric Implications
Highly Oxygenated Organic Molecules (HOM) from Gas-Phase Autoxidation Involving Peroxy Radicals: A Key Contributor to Atmospheric Aerosol
Molecular Composition and Volatility of Nucleated Particles from α-Pinene Oxidation between −50 °C and +25 °C
Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors
Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range
New particle formation in the sulfuric acid–dimethylamine–water system: reevaluation of CLOUD chamber measurements and comparison to an aerosol nucleation and growth model
Causes and importance of new particle formation in the present‐day and preindustrial atmospheres
The role of low-volatility organic compounds in initial particle growth in the atmosphere
Ion-induced nucleation of pure biogenic particles
Global atmospheric particle formation from CERN CLOUD measurements
Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formation
Source characterization of highly oxidized multifunctional compounds in a boreal forest environment using positive matrix factorization
The effect of acid–base clustering and ions on the growth of atmospheric nano-particles
Experimental particle formation rates spanning tropospheric sulfuric acid and ammonia abundances, ion production rates, and temperatures
A large source of low-volatility secondary organic aerosol