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Title Molecular understanding of sulphuric acid-amine particle nucleation in the atmosphere
Author(s) Almeida, João (Goethe U., Frankfurt ; CERN) ; Schobesberger, Siegfried (Helsinki U.) ; Kürten, Andreas (Goethe U., Frankfurt) ; Ortega, Ismael K (Helsinki U.) ; Kupiainen-Määttä, Oona (Helsinki U.) ; Praplan, Arnaud P (PSI, Villigen) ; Adamov, Alexey (Helsinki U.) ; Amorim, Antonio (U. Lisbon ; U. Beira Int., Lisbon) ; Bianchi, Federico (PSI, Villigen) ; Breitenlechner, Martin (U. Innsbruck) ; David, André (CERN) ; Dommen, Josef (PSI, Villigen) ; Donahue, Neil M (Carnegie Mellon U., Atmos. Part. Studies) ; Downard, Andrew (Caltech, Pasadena, Div. Chem.) ; Dunne, Eimear (U. Leeds, Earth and Environ.) ; Duplissy, Jonathan (Helsinki U.) ; Ehrhart, Sebastian (Goethe U., Frankfurt) ; Flagan, Richard C (Caltech, Pasadena, Div. Chem.) ; Franchin, Alessandro (Helsinki U.) ; Guida, Roberto (CERN) ; Hakala, Jani (Helsinki U.) ; Hansel, Armin (U. Innsbruck) ; Heinritzi, Martin (U. Innsbruck) ; Henschel, Henning (Helsinki U.) ; Jokinen, Tuija (Helsinki U.) ; Junninen, Heikki (Helsinki U.) ; Kajos, Maija (Helsinki U.) ; Kangasluoma, Juha (Helsinki U.) ; Keskinen, Helmi (Kuopio U.) ; Kupc, Agnieszka (U. Vienna) ; Kurtén, Theo (Helsinki U., Dept. Chem.) ; Kvashin, Alexander N (Lebedev Inst., Solar and Cosmic Ray Res. Lab.) ; Laaksonen, Ari (Kuopio U. ; Finnish Meteorological Inst.) ; Lehtipalo, Katrianne (Helsinki U.) ; Leiminger, Markus (Goethe U., Frankfurt) ; Leppä, Johannes (Finnish Meteorological Inst.) ; Loukonen, Ville (Helsinki U.) ; Makhmutov, Vladimir (Lebedev Inst., Solar and Cosmic Ray Res. Lab.) ; Mathot, Serge (CERN) ; McGrath, Matthew J (Kyoto U., Dept. Biophys.) ; Nieminen, Tuomo (Helsinki U. ; Helsinki Inst. of Phys.) ; Olenius, Tinja (Helsinki U.) ; Onnela, Antti (CERN) ; Petäjä, Tuukka (Helsinki U.) ; Riccobono, Francesco (PSI, Villigen) ; Riipinen, Ilona (Stockholm U., Dept. Appl. Environ. Sci.) ; Rissanen, Matti (Helsinki U.) ; Rondo, Linda (Goethe U., Frankfurt) ; Ruuskanen, Taina (Helsinki U.) ; Santos, Filipe D (U. Lisbon ; U. Beira Int., Lisbon) ; Sarnela, Nina (Helsinki U.) ; Schallhart, Simon (Helsinki U.) ; Schnitzhofer, Ralf (U. Innsbruck) ; Seinfeld, John H (Caltech, Pasadena, Div. Chem.) ; Simon, Mario (Goethe U., Frankfurt) ; Sipilä, Mikko (Helsinki U. ; Helsinki Inst. of Phys.) ; Stozhkov, Yuri (Lebedev Inst., Solar and Cosmic Ray Res. Lab.) ; Stratmann, Frank (Leibniz Inst. Tropospheric, Leibniz) ; Tomé, Antonio (U. Lisbon ; U. Beira Int., Lisbon) ; Tröstl, Jasmin (PSI, Villigen) ; Tsagkogeorgas, Georgios (Leibniz Inst. Tropospheric, Leibniz) ; Vaattovaara, Petri (Kuopio U.) ; Viisanen, Yrjo (Finnish Meteorological Inst.) ; Virtanen, Annele (Kuopio U.) ; Vrtala, Aron (U. Vienna) ; Wagner, Paul E (U. Vienna) ; Weingartner, Ernest (PSI, Villigen) ; Wex, Heike (Leibniz Inst. Tropospheric, Leibniz) ; Williamson, Christina (Goethe U., Frankfurt) ; Wimmer, Daniela (Goethe U., Frankfurt ; Helsinki U.) ; Ye, Penglin (Carnegie Mellon U., Atmos. Part. Studies) ; Yli-Juuti, Taina (Helsinki U.) ; Carslaw, Kenneth S (U. Leeds, Earth and Environ.) ; Kulmala, Markku (Helsinki U. ; Helsinki Inst. of Phys.) ; Curtius, Joachim (Goethe U., Frankfurt) ; Baltensperger, Urs (PSI, Villigen) ; (Helsinki U. ; Kuopio U. ; Finnish Meteorological Inst. ; Aerodyne Research, Billerica) ; Vehkamaki, Hanna (Helsinki U.) ; Kirkby, Jasper (Goethe U., Frankfurt ; CERN)
Publication 2013
Number of pages 11
In: Nature 502 (2013) 359-363
DOI 10.1038/nature12663
Subject category Chemical Physics and Chemistry
Accelerator/Facility, Experiment CERN PS ; CLOUD PS215
Abstract Nucleation of aerosol particles from trace atmospheric vapours is thought to provide up to half of global cloud condensation nuclei. Aerosols can cause a net cooling of climate by scattering sunlight and by leading to smaller but more numerous cloud droplets, which makes clouds brighter and extends their lifetimes. Atmospheric aerosols derived from human activities are thought to have compensated for a large fraction of the warming caused by greenhouse gases. However, despite its importance for climate, atmospheric nucleation is poorly understood. Recently, it has been shown that sulphuric acid and ammonia cannot explain particle formation rates observed in the lower atmosphere. It is thought that amines may enhance nucleation, but until now there has been no direct evidence for amine ternary nucleation under atmospheric conditions. Here we use the CLOUD (Cosmics Leaving OUtdoor Droplets) chamber at CERN and find that dimethylamine above three parts per trillion by volume can enhance particle formation rates more than 1,000-fold compared with ammonia, sufficient to account for the particle formation rates observed in the atmosphere. Molecular analysis of the clusters reveals that the faster nucleation is explained by a base-stabilization mechanism involving acid–amine pairs, which strongly decrease evaporation. The ion-induced contribution is generally small, reflecting the high stability of sulphuric acid–dimethylamine clusters and indicating that galactic cosmic rays exert only a small influence on their formation, except at low overall formation rates. Our experimental measurements are well reproduced by a dynamical model based on quantum chemical calculations of binding energies of molecular clusters, without any fitted parameters. These results show that, in regions of the atmosphere near amine sources, both amines and sulphur dioxide should be considered when assessing the impact of anthropogenic activities on particle formation.
Copyright/License publication: © 2013-2024 Macmillan Publishers Limited (License: CC-BY-NC-SA 3.0)

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