Now showing items 1-2 of 2

    • Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors 

      Lehtipalo, K; Yan, C; Dada, L; Bianchi, F; Xiao, M; Wagner, R; Stolzenburg, D; Ahonen, LR; Amorim, A; Baccarini, A; Bauer, PS; Baumgartner, B; Bergen, A; Bernhammer, A; Breitenlechner, M; Brilke, S; Buchholz, A; Mazon, SB; Chen, D; Chen, X; et al [Incl Nieminen, T; Virtanen, A; Väisänen, O; Ylisirniö, A] (American Association for the Advancement of Science (AAAS), 2018)
      A major fraction of atmospheric aerosol particles, which affect both air quality and climate, form from gaseous precursors in the atmosphere. Highly oxygenated organic molecules (HOMs), formed by oxidation of biogenic ...
    • Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range 

      Stolzenburg, D; Fischer, L; Vogel, AL; Heinritzi, M; Schervish, M; Simon, M; Wagner, AC; Dada, L; Ahonen, LR; Amorim, A; Baccarini, A; Bauer, PS; Baumgartner, B; Bergen, A; Bianchi, F; Breitenlechner, M; Brilke, S; Buenrostro Mazon, S; Chen, D; Dias, A (Proceedings of the National Academy of Sciences, 2018)
      Nucleation and growth of aerosol particles from atmospheric vapors constitutes a major source of global cloud condensation nuclei (CCN). The fraction of newly formed particles that reaches CCN sizes is highly sensitive to ...