Lubna Dada

Värske

• Diurnal evolution of negative atmospheric ions above the boreal forest: from ground level to the free troposphere
• Quiet New Particle Formation in the Atmosphere
• Terpene emissions from boreal wetlands can initiate stronger atmospheric new particle formation than boreal forests
• Molecular Composition of Oxygenated Organic Molecules and Their Contributions to Organic Aerosol in Beijing
• The Synergistic Role of Sulfuric Acid, Bases, and Oxidized Organics Governing New-Particle Formation in Beijing
• Is reducing new particle formation a plausible solution to mitigate particulate air pollution in Beijing and other Chinese megacities?
• Role of iodine oxoacids in atmospheric aerosol nucleation
• Particle growth with photochemical age from new particle formation to haze in the winter of Beijing, China
• Refined classification and characterization of atmospheric new-particle formation events using air ions
• The role of H2SO4-NH3 anion clusters in ion-induced aerosol nucleation mechanisms in the boreal forest
• Observations of biogenic ion-induced cluster formation in the atmosphere
• Influence of temperature on the molecular composition of ions and charged clusters during pure biogenic nucleation