Joao Almeida, Siegfried Schobesberger, Christoph Andreas Kürten, Ismael K. Ortega, Oona Kupiainen-Määttä, Arnaud Patrick Praplan, Alexey Adamov, Antonio Amorim, Federico Bianchi, Martin Breitenlechner, André David, Josef Dommen, Neil McPherson Donahue, Andrew Downard, Eimear M. Dunne, Jonathan Duplissy, Sebastian Ehrhart, Richard C. Flagan, Alessandro Franchin, Roberto Guida, Jani Hakala, Armin Hansel, Martin Heinritzi, Henning Henschel, Tuija Jokinen, Heikki Junninen, Maija Kajos, Juha Kangasluoma, Helmi Keskinen, Agnieszka Kupc, Theo Kurtén, Alexander N. Kvashin, Ari Laaksonen, Katrianne Lehtipalo, Markus Leiminger, Johannes Leppä, Ville Loukonen, Vladimir Makhmutov, Serge Mathot, Matthew J. McGrath, Tuomo Nieminen, Tinja Olenius, Antti Onnela, Tuukka Petäjä, Francesco Riccobono, Ilona Riipinen, Matti P. Rissanen, Linda Rondo, Taina Ruuskanen, Filipe Duarte Santos, Nina Sarnela, Simon Schallhart, Ralf Schnitzhofer, John H. Seinfeld, Mario Simon, Mikko Sipilä, Yuri Stozhkov, Frank Stratmann, Antonio Tomé, Jasmin Tröstl, Georgios Tsagkogeorgas, Petri Vaattovaara, Yrjo Viisanen, Annele Virtanen, Aron Vrtala, Paul E. Wagner, Ernest Weingartner, Heike Wex, Christina Williamson, Daniela Wimmer, Penglin Ye, Taina Yli-Juuti, Kenneth S. Carslaw, Markku Kulmala, Joachim Curtius, Urs Baltensperger, Douglas R. Worsnop, Hanna Vehkamäki, Jasper Kirkby
- 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.
MetadatenAuthor: | Joao Almeida, Siegfried SchobesbergerORCiDGND, Christoph Andreas KürtenORCiDGND, Ismael K. Ortega, Oona Kupiainen-Määttä, Arnaud Patrick Praplan, Alexey Adamov, Antonio AmorimORCiD, Federico BianchiORCiDGND, Martin BreitenlechnerORCiD, André David, Josef Dommen, Neil McPherson DonahueORCiDGND, Andrew Downard, Eimear M. Dunne, Jonathan DuplissyORCiD, Sebastian Ehrhart, Richard C. FlaganORCiD, Alessandro Franchin, Roberto Guida, Jani Hakala, Armin HanselORCiD, Martin HeinritziORCiDGND, Henning Henschel, Tuija Jokinen, Heikki Junninen, Maija Kajos, Juha Kangasluoma, Helmi Keskinen, Agnieszka Kupc, Theo KurténORCiD, Alexander N. Kvashin, Ari Laaksonen, Katrianne LehtipaloORCiDGND, Markus Leiminger, Johannes Leppä, Ville Loukonen, Vladimir MakhmutovORCiD, Serge Mathot, Matthew J. McGrath, Tuomo Nieminen, Tinja Olenius, Antti OnnelaORCiD, Tuukka Petäjä, Francesco Riccobono, Ilona RiipinenORCiD, Matti P. RissanenORCiD, Linda Rondo, Taina Ruuskanen, Filipe Duarte Santos, Nina Sarnela, Simon Schallhart, Ralf Schnitzhofer, John H. Seinfeld, Mario SimonORCiD, Mikko SipiläORCiD, Yuri Stozhkov, Frank StratmannORCiDGND, Antonio Tomé, Jasmin Tröstl, Georgios Tsagkogeorgas, Petri Vaattovaara, Yrjo Viisanen, Annele VirtanenORCiD, Aron Vrtala, Paul E. Wagner, Ernest Weingartner, Heike WexORCiDGND, Christina Williamson, Daniela WimmerORCiDGND, Penglin Ye, Taina Yli-Juuti, Kenneth S. Carslaw, Markku KulmalaORCiDGND, Joachim CurtiusORCiD, Urs BaltenspergerORCiDGND, Douglas R. WorsnopORCiD, Hanna Vehkamäki, Jasper KirkbyORCiD |
---|
URN: | urn:nbn:de:hebis:30:3-318032 |
---|
DOI: | https://doi.org/10.1038/nature12663 |
---|
ISSN: | 0028-0836 |
---|
ISSN: | 1476-4687 |
---|
Pubmed Id: | https://pubmed.ncbi.nlm.nih.gov/24097350 |
---|
Parent Title (English): | Nature |
---|
Publisher: | Nature Publising Group |
---|
Place of publication: | London [u.a.] |
---|
Document Type: | Article |
---|
Language: | English |
---|
Date of Publication (online): | 2013/10/06 |
---|
Date of first Publication: | 2013/10/06 |
---|
Publishing Institution: | Universitätsbibliothek Johann Christian Senckenberg |
---|
Release Date: | 2013/11/22 |
---|
Issue: | 502 |
---|
Page Number: | 11 |
---|
First Page: | 359 |
---|
Last Page: | 363 |
---|
Note: | This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/3.0/ |
---|
HeBIS-PPN: | 363161600 |
---|
Institutes: | Geowissenschaften / Geographie / Geowissenschaften |
---|
Dewey Decimal Classification: | 5 Naturwissenschaften und Mathematik / 55 Geowissenschaften, Geologie / 550 Geowissenschaften |
---|
Sammlungen: | Universitätspublikationen |
---|
Licence (German): | Creative Commons - Namensnennung-Keine kommerzielle Nutzung-Weitergabe unter gleichen Bedingungen |
---|