Corrigendum to "Particle hygroscopicity during atmospheric new particle formation events: implications for the chemical species contributing to particle growth" published in Atmos. Chem. Phys., 13, 6637–6646, 2013

According to our results, the mixing is stronger on observed event than on nonevent days which leads to higher saturation ratio of organic vapors due to the vertical motion. The

In order to investigate the atmospheric particle formation and growth processes, and to quantify the particle number (PN) concentration and size distributions in Hong Kong,

Considering ion–particle interactions by applying theoret- ical parameterizations of the attachment and recombination processes to the combined NAIS and mobility particle

signed case studies corresponding to representative (in terms of the observed ranges of sulfuric acid gas concentrations, concentrations and charged fractions of freshly nu-

Based on these measurements, the hygroscopic parameter κ , and the ZSR mixing rule was used to examine the relationship between the particle hygroscopic growth, the CCN activity,

From 25 November 2013 to 25 January 2014, a combination of one nano-CNC, one nano-SPMS, and one long-SPMS has been utilized to investigate atmospheric nucle- ation by measuring

Schematic representation of physical model for polypropylene particle growth (a. micro-particle distribution within the initial macro-particle).. For the two types of

presents dynamical and chemical evolutions in the mass and size distributions of aerosols due to emissions, new particle formation, condensation, Brownian coagula- tion, dry