Activation of sub-3 nm organic particles in the particle size magnifier using humid and dry conditions |
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artikull shkencor i botuar në vitin 2022 |
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Automated identification of local contamination in remote atmospheric composition time series |
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A central arctic extreme aerosol event triggered by a warm air-mass intrusion |
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Chemical composition of nanoparticles from α-pinene nucleation and the influence of isoprene and relative humidity at low temperature |
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Deposition potential of 0.003–10 µm ambient particles in the humidified human respiratory tract: Contribution of new particle formation events in Beijing |
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Diurnal evolution of negative atmospheric ions above the boreal forest: from ground level to the free troposphere |
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The driving factors of new particle formation and growth in the polluted boundary layer |
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The effect of COVID-19 restrictions on atmospheric new particle formation in Beijing |
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An evaluation of new particle formation events in Helsinki during a Baltic Sea cyanobacterial summer bloom |
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Formation and growth of sub-3-nm aerosol particles in experimental chambers |
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Formation of nighttime sulfuric acid from the ozonolysis of alkenes in Beijing |
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A full year of aerosol size distribution data from the central Arctic under an extreme positive Arctic Oscillation: insights from the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition |
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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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Influence of Aerosol Chemical Composition on Condensation Sink Efficiency and New Particle Formation in Beijing |
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Influence of temperature on the molecular composition of ions and charged clusters during pure biogenic nucleation |
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Insights into vertical differences of particle number size distributions in winter in Beijing, China |
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Is reducing new particle formation a plausible solution to mitigate particulate air pollution in Beijing and other Chinese megacities? |
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Measurement report: A multi-year study on the impacts of Chinese New Year celebrations on air quality in Beijing, China |
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The missing base molecules in atmospheric acid-base nucleation |
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Molecular Composition and Volatility of Nucleated Particles from α-Pinene Oxidation between -50 °C and +25 °C |
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Molecular Composition of Oxygenated Organic Molecules and Their Contributions to Organic Aerosol in Beijing |
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Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors |
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Observations of biogenic ion-induced cluster formation in the atmosphere. |
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Observed coupling between air mass history, secondary growth of nucleation mode particles and aerosol pollution levels in Beijing |
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Photo-oxidation of aromatic hydrocarbons produces low-volatility organic compounds |
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Physical and Chemical Properties of Cloud Droplet Residuals and Aerosol Particles During the Arctic Ocean 2018 Expedition |
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A Predictive Model for Steady State Ozone Concentration at an Urban-Coastal Site |
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Rapid growth of new atmospheric particles by nitric acid and ammonia condensation |
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Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range |
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Rapid mass growth and enhanced light extinction of atmospheric aerosols during the heating season haze episodes in Beijing revealed by aerosol–chemistry–radiation–boundary layer interaction |
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The role of H<sub>2</sub>SO<sub>4</sub>-NH<sub>3</sub> anion clusters in ion-induced aerosol nucleation mechanisms in the boreal forest |
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Substantial contribution of iodine to Arctic ozone destruction |
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Supplementary material to "New particle formation at urban and high-altitude remote sites in the south-eastern Iberian Peninsula" |
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Survival of newly formed particles in haze conditions |
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Synergistic HNO3–H2SO4–NH3 upper tropospheric particle formation |
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The Synergistic Role of Sulfuric Acid, Bases, and Oxidized Organics Governing New-Particle Formation in Beijing |
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Towards understanding the characteristics of new particle formation in the Eastern Mediterranean |
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Vertical characterization of highly oxygenated molecules (HOMs) below and above a boreal forest canopy |
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What controls the observed size-dependency of the growth rates of sub-10 nm atmospheric particles? |
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