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| Assessing the importance of nitric acid and ammonia for particle growth in the polluted boundary layer
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| Temperature, humidity, and ionisation effect of iodine oxoacid nucleation
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| An intercomparison study of four different techniques for measuring the chemical composition of nanoparticles
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| Role of sesquiterpenes in biogenic new particle formation
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| The gas-phase formation mechanism of iodic acid as an atmospheric aerosol source
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| Iodine oxoacids enhance nucleation of sulfuric acid particles in the atmosphere
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| Measurement of the collision rate coefficients between atmospheric ions and multiply charged aerosol particles in the CERN CLOUD chamber
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| Molecular understanding of the enhancement in organic aerosol mass at high relative humidity
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| Survival of newly formed particles in haze conditions
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| High gas-phase methanesulfonic acid production in the OH-initiated oxidation of dimethyl sulfide at low temperatures
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| Synergistic HNO<sub>3</sub>-H<sub>2</sub>SO<sub>4</sub>-NH<sub>3</sub> upper tropospheric particle formation
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| Chemical composition of nanoparticles from <em>α</em>-pinene nucleation and the influence of isoprene and relative humidity at low temperature
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| Determination of the collision rate coefficient between charged iodic acid clusters and iodic acid using the appearance time method
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| Role of iodine oxoacids in atmospheric aerosol nucleation
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| The driving factors of new particle formation and growth in the polluted boundary layer
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| Molecular understanding of the suppression of new-particle formation by isoprene
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| Molecular understanding of new-particle formation from <em>α</em>-pinene between -50 and +25 °C
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| Enhanced growth rate of atmospheric particles from sulfuric acid
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| Rapid growth of new atmospheric particles by nitric acid and ammonia condensation
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