Area of research
Atmospheric Science · Global and Planetary Change
Research interest
Research interests include Chemistry, Aerosol, Sulfuric acid, Environmental chemistry, Particle (ecology), and Atmospheric sciences.
Anthropogenic organic aerosol in Europe produced mainly through second-generation oxidation
Post-marketing safety surveillance for the recombinant zoster vaccine (Shingrix), vaccine adverse event reporting system, United States, October 2017–April 2024
The impact of ammonia on particle formation in the Asian Tropopause Aerosol Layer
Iodine oxoacids enhance nucleation of sulfuric acid particles in the atmosphere
Molecular Understanding of the Enhancement in Organic Aerosol Mass at High Relative Humidity
NO at low concentration can enhance the formation of highly oxygenated biogenic molecules in the atmosphere
Widespread detection of chlorine oxyacids in the Arctic atmosphere
Synergistic HNO3–H2SO4–NH3 upper tropospheric particle formation
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
Critical Role of Iodous Acid in Neutral Iodine Oxoacid Nucleation
The effect of COVID-19 restrictions on atmospheric new particle formation in Beijing
Role of iodine oxoacids in atmospheric aerosol nucleation
The Synergistic Role of Sulfuric Acid, Bases, and Oxidized Organics Governing New‐Particle Formation in Beijing
The driving factors of new particle formation and growth in the polluted boundary layer
Molecular Composition of Oxygenated Organic Molecules and Their Contributions to Organic Aerosol in Beijing
Rapid growth of new atmospheric particles by nitric acid and ammonia condensation
Differing Mechanisms of New Particle Formation at Two Arctic Sites
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
Molecular understanding of the suppression of new-particle formation by isoprene
Formation of highly oxygenated organic molecules from chlorine-atom-initiated oxidation of alpha-pinene
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