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DOI10.1126/science.aaf2649
Global atmospheric particle formation from CERN CLOUD measurements
Dunne E.M.; Gordon H.; Kürten A.; Almeida J.; Duplissy J.; Williamson C.; Ortega I.K.; Pringle K.J.; Adamov A.; Baltensperger U.; Barmet P.; Benduhn F.; Bianchi F.; Breitenlechner M.; Clarke A.; Curtius J.; Dommen J.; Donahue N.M.; Ehrhart S.; Flagan R.C.; Franchin A.; Guida R.; Hakala J.; Hansel A.; Heinritzi M.; Jokinen T.; Kangasluoma J.; Kirkby J.; Kulmala M.; Kupc A.; Lawler M.J.; Lehtipalo K.; Makhmutov V.; Mann G.; Mathot S.; Merikanto J.; Miettinen P.; Nenes A.; Onnela A.; Rap A.; Reddington C.L.S.; Riccobono F.; Richards N.A.D.; Rissanen M.P.; Rondo L.; Sarnela N.; Schobesberger S.; Sengupta K.; Simon M.; Sipilä M.; Smith J.N.; Stozkhov Y.; Tomé A.; Tröstl J.; Wagner P.E.; Wimmer D.; Winkler P.M.; Worsnop D.R.; Carslaw K.S.
发表日期2016
ISSN0036-8075
起始页码1119
结束页码1124
卷号354期号:6316
英文摘要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. Copyright © 2016 by the American Association for the Advancement of Science.
英文关键词ammonia; ion; organic compound; sulfuric acid; aerosol; aerosol formation; atmospheric chemistry; atmospheric particle; concentration (composition); cosmic ray; flux chamber; global perspective; laboratory method; measurement method; nucleation; organic compound; reaction kinetics; aerosol; Article; astronomy; atmosphere; climate; controlled study; gas; kinetics; measurement; particle size; priority journal; simulation
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/243585
作者单位School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, United Kingdom; European Organization for Nuclear Research (CERN), Geneva, 1211, Switzerland; Goethe-University Frankfurt am Main, Institute for Atmospheric and Environmental Sciences, Altenhöferallee 1, Frankfurt am Main, 60438, Germany; Helsinki Institute of Physics, Helsinki, FI-00014, Finland; Laboratoire de Physique des Lasers, Atomes et Molécules (PhLAM), Université Lille 1, UMR 8523 CNRS, Villeneuve d'Ascq, 59655, France; Department of Physics, University of Helsinki, Post Office Box 64, Helsinki, FI-00014, Finland; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, 5232, Switzerland; Institute for Advanced Sustainability Studies, Berliner Straße 130, Potsdam, D-14467, Germany; Institute of Ion Physics and Applied Physics, Leopold-Franzens University, Technikerstraße 25, Innsbruck, 6020, Austria; Department of Oceanography, University of Hawaii, 1000 Pope Road, Honolulu, HI 96822, United States; Center for A...
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Dunne E.M.,Gordon H.,Kürten A.,et al. Global atmospheric particle formation from CERN CLOUD measurements[J],2016,354(6316).
APA Dunne E.M..,Gordon H..,Kürten A..,Almeida J..,Duplissy J..,...&Carslaw K.S..(2016).Global atmospheric particle formation from CERN CLOUD measurements.Science,354(6316).
MLA Dunne E.M.,et al."Global atmospheric particle formation from CERN CLOUD measurements".Science 354.6316(2016).
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