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Proceedings of the National Academy of Sciences of the United States of America|October 27, 2025
Global impact of anthropogenic NH<sub>3</sub> emissions on upper tropospheric aerosol formationChristos Xenofontos, Matthias Kohl, Samuel Ruhl, et al.Science (New York, N.Y.)|November 3, 2016
Global atmospheric particle formation from CERN CLOUD measurementsEimear M Dunne, Hamish Gordon, Andreas Kürten, et al.Proceedings of the National Academy of Sciences of the United States of America|August 30, 2018
Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature rangeDominik Stolzenburg, Lukas Fischer, Alexander L Vogel, et al.Nature|May 27, 2016
The role of low-volatility organic compounds in initial particle growth in the atmosphereJasmin Tröstl, Wayne K Chuang, Hamish Gordon, et al.Nature|December 5, 2024
New particle formation from isoprene under upper-tropospheric conditionsJiali Shen, Douglas M Russell, Jenna DeVivo, et al.Nature|May 18, 2022
Synergistic HNO<sub>3</sub>-H<sub>2</sub>SO<sub>4</sub>-NH<sub>3</sub> upper tropospheric particle formationMingyi Wang, Mao Xiao, Barbara Bertozzi, et al.Proceedings of the National Academy of Sciences of the United States of America|October 30, 2016
Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formationHamish Gordon, Kamalika Sengupta, Alexandru Rap, et al.Nature|May 27, 2016
Ion-induced nucleation of pure biogenic particlesJasper Kirkby, Jonathan Duplissy, Kamalika Sengupta, et al.Environmental Science: Atmospheres|June 24, 2026
Nucleation of α-pinene oxidation products with sulfuric acidEva Sommer, João Almeida, Wenjuan Yu, et al.Science Advances|December 15, 2018
Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vaporsKatrianne Lehtipalo, Chao Yan, Lubna Dada, et al.Pageof 2