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Global atmospheric particle formation from CERN CLOUD measurements
Author(s) -
E. M. Dunne,
Hamish Gordon,
Andreas Kürten,
J. Almeida,
Jonathan Duplissy,
Christina Williamson,
Ismaël K. Ortega,
K. J. Pringle,
Alexey Adamov,
Urs Baltensperger,
P. Barmet,
François Benduhn,
Federico Bianchi,
Martin Breitenlechner,
A. D. Clarke,
Joachim Curtius,
Josef Dommen,
Neil M. Donahue,
Sebastian Ehrhart,
Richard C. Flagan,
Alessandro Franchin,
R. Guida,
Jani Hakala,
Armin Hansel,
Martin Heinritzi,
Tuija Jokinen,
Juha Kangasluoma,
J. Kirkby,
Markku Kulmala,
Agnieszka Kupc,
Michael J. Lawler,
Katrianne Lehtipalo,
В. С. Махмутов,
G. W. Mann,
Serge Mathot,
Joonas Merikanto,
Pasi Miettinen,
Athanasios Nenes,
Antti Onnela,
Alexandru Rap,
Carly Reddington,
Francesco Riccobono,
N. A. D. Richards,
Matti Rissanen,
L. Rondo,
Nina Sarnela,
Siegfried Schobesberger,
Kamalika Sengupta,
Mario Simon,
Mikko Sipilä,
James N. Smith,
Yuri Stozkhov,
António Tomé,
Jasmin Tröstl,
Paul Wagner,
Daniela Wimmer,
Paul M. Winkler,
Douglas R. Worsnop,
K. S. Carslaw
Publication year - 2016
Publication title -
science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 12.556
H-Index - 1186
eISSN - 1095-9203
pISSN - 0036-8075
DOI - 10.1126/science.aaf2649
Subject(s) - large hadron collider , cloud computing , particle (ecology) , cloud chamber , physics , atmospheric sciences , environmental science , meteorology , nuclear physics , geology , computer science , oceanography , operating system
Fundamental questions remain about the origin of newly formed atmospheric aerosol particles because data from laboratory measurements have been insufficient to build global models. In contrast, gas-phase chemistry models have been based on laboratory kinetics measurements for decades. We built a global model of aerosol formation by using extensive laboratory measurements of rates of nucleation involving sulfuric acid, ammonia, ions, and organic compounds conducted in the CERN CLOUD (Cosmics Leaving Outdoor Droplets) chamber. The simulations and a comparison with atmospheric observations show that nearly all nucleation throughout the present-day atmosphere involves ammonia or biogenic organic compounds, in addition to sulfuric acid. A considerable fraction of nucleation involves ions, but the relatively weak dependence on ion concentrations indicates that for the processes studied, variations in cosmic ray intensity do not appreciably affect climate through nucleation in the present-day atmosphere.

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