TY - JOUR A1 - Stolzenburg, Dominik A1 - Fischer, Lukas A1 - Vogel, Alexander L. A1 - Heinritzi, Martin A1 - Schervish, Meredith A1 - Simon, Mario A1 - Wagner, Andrea Christine A1 - Dada, Lubna A1 - Ahonen, Lauri R. A1 - Amorim, Antonio A1 - Baccarini, Andrea A1 - Bauer, Paulus Salomon A1 - Baumgartner, Bernhard A1 - Bergen, Anton A1 - Bianchi, Federico A1 - Breitenlechner, Martin A1 - Brilke, Sophia A1 - Buenrostro Mazon, Stephany A1 - Chen, Dexian A1 - Dias, Antonio A1 - Draper, Danielle C. A1 - Duplissy, Jonathan A1 - El Haddad, Imad A1 - Finkenzeller, Henning A1 - Frege, Carla A1 - Fuchs, Claudia A1 - Garmash, Olga A1 - Gordon, Hamish A1 - He, Xucheng A1 - Helm, Johanna A1 - Hofbauer, Victoria A1 - Hoyle, Christopher Robert A1 - Kim, Changhyuk A1 - Kirkby, Jasper A1 - Kontkanen, Jenni A1 - Kürten, Christoph Andreas A1 - Lampilahti, Janne A1 - Lawler, Michael Joseph A1 - Lehtipalo, Katrianne A1 - Leiminger, Markus A1 - Mai, Huajun A1 - Mathot, Serge A1 - Mentler, Bernhard A1 - Molteni, Ugo A1 - Nie, Wei A1 - Nieminen, Tuomo A1 - Nowak, John B. A1 - Ojdanic, Andrea A1 - Onnela, Antti A1 - Passananti, Monica A1 - Petäjä, Tuukka A1 - Quéléver, Lauriane L. J. A1 - Rissanen, Matti P. A1 - Sarnela, Nina A1 - Schallhart, Simon A1 - Tauber, Christian A1 - Tomé, Antonio A1 - Wagner, Robert A1 - Wang, Mingyi A1 - Weitz, Lena A1 - Wimmer, Daniela A1 - Xiao, Mao A1 - Yan, Chao A1 - Ye, Penglin A1 - Zha, Qiaozhi A1 - Baltensperger, Urs A1 - Curtius, Joachim A1 - Dommen, Josef A1 - Flagan, Richard C. A1 - Kulmala, Markku A1 - Smith, James N. A1 - Worsnop, Douglas R. A1 - Hansel, Armin A1 - Donahue, Neil McPherson A1 - Winkler, Paul M. T1 - Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range T2 - Proceedings of the National Academy of Sciences of the United States of America N2 - 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 particle growth rates, especially for particle sizes <10 nm, where coagulation losses to larger aerosol particles are greatest. Recent results show that some oxidation products from biogenic volatile organic compounds are major contributors to particle formation and initial growth. However, whether oxidized organics contribute to particle growth over the broad span of tropospheric temperatures remains an open question, and quantitative mass balance for organic growth has yet to be demonstrated at any temperature. Here, in experiments performed under atmospheric conditions in the Cosmics Leaving Outdoor Droplets (CLOUD) chamber at the European Organization for Nuclear Research (CERN), we show that rapid growth of organic particles occurs over the range from −25 ∘C to 25 ∘C. The lower extent of autoxidation at reduced temperatures is compensated by the decreased volatility of all oxidized molecules. This is confirmed by particle-phase composition measurements, showing enhanced uptake of relatively less oxygenated products at cold temperatures. We can reproduce the measured growth rates using an aerosol growth model based entirely on the experimentally measured gas-phase spectra of oxidized organic molecules obtained from two complementary mass spectrometers. We show that the growth rates are sensitive to particle curvature, explaining widespread atmospheric observations that particle growth rates increase in the single-digit-nanometer size range. Our results demonstrate that organic vapors can contribute to particle growth over a wide range of tropospheric temperatures from molecular cluster sizes onward. KW - aerosols KW - nanoparticle growth KW - aerosol formation KW - CLOUD experiment KW - volatile organic compounds Y1 - 2018 UR - http://publikationen.ub.uni-frankfurt.de/frontdoor/index/index/docId/47734 UR - https://nbn-resolving.org/urn:nbn:de:hebis:30:3-477347 SN - 1091-6490 SN - 0027-8424 N1 - This open access article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND). VL - 115 IS - 37 SP - 9122 EP - 9127 PB - National Acad. of Sciences CY - Washington, DC ER -