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  • 1
    Publication Date: 2013-02-23
    Description: Atmospheric nucleation is the dominant source of aerosol particles in the global atmosphere and an important player in aerosol climatic effects. The key steps of this process occur in the sub-2-nanometer (nm) size range, in which direct size-segregated observations have not been possible until very recently. Here, we present detailed observations of atmospheric nanoparticles and clusters down to 1-nm mobility diameter. We identified three separate size regimes below 2-nm diameter that build up a physically, chemically, and dynamically consistent framework on atmospheric nucleation--more specifically, aerosol formation via neutral pathways. Our findings emphasize the important role of organic compounds in atmospheric aerosol formation, subsequent aerosol growth, radiative forcing and associated feedbacks between biogenic emissions, clouds, and climate.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Kulmala, Markku -- Kontkanen, Jenni -- Junninen, Heikki -- Lehtipalo, Katrianne -- Manninen, Hanna E -- Nieminen, Tuomo -- Petaja, Tuukka -- Sipila, Mikko -- Schobesberger, Siegfried -- Rantala, Pekka -- Franchin, Alessandro -- Jokinen, Tuija -- Jarvinen, Emma -- Aijala, Mikko -- Kangasluoma, Juha -- Hakala, Jani -- Aalto, Pasi P -- Paasonen, Pauli -- Mikkila, Jyri -- Vanhanen, Joonas -- Aalto, Juho -- Hakola, Hannele -- Makkonen, Ulla -- Ruuskanen, Taina -- Mauldin, Roy L 3rd -- Duplissy, Jonathan -- Vehkamaki, Hanna -- Back, Jaana -- Kortelainen, Aki -- Riipinen, Ilona -- Kurten, Theo -- Johnston, Murray V -- Smith, James N -- Ehn, Mikael -- Mentel, Thomas F -- Lehtinen, Kari E J -- Laaksonen, Ari -- Kerminen, Veli-Matti -- Worsnop, Douglas R -- New York, N.Y. -- Science. 2013 Feb 22;339(6122):943-6. doi: 10.1126/science.1227385.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Physics, University of Helsinki, Finland. markku.kulmala@helsinki.fi〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23430652" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2012-08-10
    Description: Atmospheric oxidation is a key phenomenon that connects atmospheric chemistry with globally challenging environmental issues, such as climate change, stratospheric ozone loss, acidification of soils and water, and health effects of air quality. Ozone, the hydroxyl radical and the nitrate radical are generally considered to be the dominant oxidants that initiate the removal of trace gases, including pollutants, from the atmosphere. Here we present atmospheric observations from a boreal forest region in Finland, supported by laboratory experiments and theoretical considerations, that allow us to identify another compound, probably a stabilized Criegee intermediate (a carbonyl oxide with two free-radical sites) or its derivative, which has a significant capacity to oxidize sulphur dioxide and potentially other trace gases. This compound probably enhances the reactivity of the atmosphere, particularly with regard to the production of sulphuric acid, and consequently atmospheric aerosol formation. Our findings suggest that this new atmospherically relevant oxidation route is important relative to oxidation by the hydroxyl radical, at least at moderate concentrations of that radical. We also find that the oxidation chemistry of this compound seems to be tightly linked to the presence of alkenes of biogenic origin.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Mauldin, R L 3rd -- Berndt, T -- Sipila, M -- Paasonen, P -- Petaja, T -- Kim, S -- Kurten, T -- Stratmann, F -- Kerminen, V-M -- Kulmala, M -- England -- Nature. 2012 Aug 9;488(7410):193-6. doi: 10.1038/nature11278.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉University of Helsinki, Department of Physics, FI-00014 Helsinki, Finland. roy.mauldin@helsinki.fi〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22874964" target="_blank"〉PubMed〈/a〉
    Keywords: Alkenes/metabolism ; Atmosphere/*chemistry ; Finland ; Free Radicals/chemistry ; Hydroxyl Radical/chemistry ; Oxidants/*chemistry/metabolism ; Ozone/chemistry ; Sulfur Dioxide/analysis/*chemistry ; Terpenes/chemistry/metabolism ; Trees/metabolism ; Volatile Organic Compounds/analysis/chemistry/metabolism
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2010-03-06
    Description: Nucleation is a fundamental step in atmospheric new-particle formation. However, laboratory experiments on nucleation have systematically failed to demonstrate sulfuric acid particle formation rates as high as those necessary to account for ambient atmospheric concentrations, and the role of sulfuric acid in atmospheric nucleation has remained a mystery. Here, we report measurements of new particles (with diameters of approximately 1.5 nanometers) observed immediately after their formation at atmospherically relevant sulfuric acid concentrations. Furthermore, we show that correlations between measured nucleation rates and sulfuric acid concentrations suggest that freshly formed particles contain one to two sulfuric acid molecules, a number consistent with assumptions that are based on atmospheric observations. Incorporation of these findings into global models should improve the understanding of the impact of secondary particle formation on climate.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Sipila, Mikko -- Berndt, Torsten -- Petaja, Tuukka -- Brus, David -- Vanhanen, Joonas -- Stratmann, Frank -- Patokoski, Johanna -- Mauldin, Roy L 3rd -- Hyvarinen, Antti-Pekka -- Lihavainen, Heikki -- Kulmala, Markku -- New York, N.Y. -- Science. 2010 Mar 5;327(5970):1243-6. doi: 10.1126/science.1180315.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Leibniz-Institut fur Tropospharenforschung e.V., Leipzig 04318, Germany. mikko.sipila@helsinki.fi〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20203046" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2016-04-12
    Description: Nitrogen oxides are essential for the formation of secondary atmospheric aerosols and of atmospheric oxidants such as ozone and the hydroxyl radical, which controls the self-cleansing capacity of the atmosphere. Nitric acid, a major oxidation product of nitrogen oxides, has traditionally been considered to be a permanent sink of nitrogen oxides. However, model studies predict higher ratios of nitric acid to nitrogen oxides in the troposphere than are observed. A 'renoxification' process that recycles nitric acid into nitrogen oxides has been proposed to reconcile observations with model studies, but the mechanisms responsible for this process remain uncertain. Here we present data from an aircraft measurement campaign over the North Atlantic Ocean and find evidence for rapid recycling of nitric acid to nitrous acid and nitrogen oxides in the clean marine boundary layer via particulate nitrate photolysis. Laboratory experiments further demonstrate the photolysis of particulate nitrate collected on filters at a rate more than two orders of magnitude greater than that of gaseous nitric acid, with nitrous acid as the main product. Box model calculations based on the Master Chemical Mechanism suggest that particulate nitrate photolysis mainly sustains the observed levels of nitrous acid and nitrogen oxides at midday under typical marine boundary layer conditions. Given that oceans account for more than 70 per cent of Earth's surface, we propose that particulate nitrate photolysis could be a substantial tropospheric nitrogen oxide source. Recycling of nitrogen oxides in remote oceanic regions with minimal direct nitrogen oxide emissions could increase the formation of tropospheric oxidants and secondary atmospheric aerosols on a global scale.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Ye, Chunxiang -- Zhou, Xianliang -- Pu, Dennis -- Stutz, Jochen -- Festa, James -- Spolaor, Max -- Tsai, Catalina -- Cantrell, Christopher -- Mauldin, Roy L 3rd -- Campos, Teresa -- Weinheimer, Andrew -- Hornbrook, Rebecca S -- Apel, Eric C -- Guenther, Alex -- Kaser, Lisa -- Yuan, Bin -- Karl, Thomas -- Haggerty, Julie -- Hall, Samuel -- Ullmann, Kirk -- Smith, James N -- Ortega, John -- Knote, Christoph -- England -- Nature. 2016 Apr 28;532(7600):489-91. doi: 10.1038/nature17195. Epub 2016 Apr 11.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Wadsworth Center, New York State Department of Health, Albany, New York, USA. ; Department of Environmental Health Sciences, State University of New York, Albany, New York, USA. ; Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles (UCLA), California, USA. ; Department of Atmospheric and Oceanic Sciences, University of Colorado at Boulder, Boulder, Colorado, USA. ; Department of Physics, University of Helsinki, Helsinki, Finland. ; National Center for Atmospheric Research, Boulder, Colorado, USA. ; Pacific Northwest National Laboratory, Richland, Washington, USA. ; NOAA, Earth System Research Laboratory, Chemical Sciences Division, Boulder, Colorado, USA. ; Cooperative Institute for Research in Environmental Sciences, University of Colorado at Boulder, Boulder, Colorado, USA. ; Institute for Meteorology and Geophysics, University of Innsbruck, Innsbruck, Austria. ; University of Eastern Finland, Kuopio, Finland.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/27064904" target="_blank"〉PubMed〈/a〉
    Keywords: Aerosols/chemistry ; Atlantic Ocean ; Atmosphere/*chemistry ; Nitrates/analysis/chemistry ; Nitric Acid/chemistry ; Nitrogen/*analysis/*chemistry ; Nitrogen Oxides/*analysis/*chemistry ; Nitrous Acid/analysis/chemistry ; North Carolina ; Oxidants/chemistry ; Photolysis ; Seawater/*chemistry ; South Carolina
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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