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  • 1
    Publication Date: 2014-02-28
    Description: Forests emit large quantities of volatile organic compounds (VOCs) to the atmosphere. Their condensable oxidation products can form secondary organic aerosol, a significant and ubiquitous component of atmospheric aerosol, which is known to affect the Earth's radiation balance by scattering solar radiation and by acting as cloud condensation nuclei. The quantitative assessment of such climate effects remains hampered by a number of factors, including an incomplete understanding of how biogenic VOCs contribute to the formation of atmospheric secondary organic aerosol. The growth of newly formed particles from sizes of less than three nanometres up to the sizes of cloud condensation nuclei (about one hundred nanometres) in many continental ecosystems requires abundant, essentially non-volatile organic vapours, but the sources and compositions of such vapours remain unknown. Here we investigate the oxidation of VOCs, in particular the terpene alpha-pinene, under atmospherically relevant conditions in chamber experiments. We find that a direct pathway leads from several biogenic VOCs, such as monoterpenes, to the formation of large amounts of extremely low-volatility vapours. These vapours form at significant mass yield in the gas phase and condense irreversibly onto aerosol surfaces to produce secondary organic aerosol, helping to explain the discrepancy between the observed atmospheric burden of secondary organic aerosol and that reported by many model studies. We further demonstrate how these low-volatility vapours can enhance, or even dominate, the formation and growth of aerosol particles over forested regions, providing a missing link between biogenic VOCs and their conversion to aerosol particles. Our findings could help to improve assessments of biosphere-aerosol-climate feedback mechanisms, and the air quality and climate effects of biogenic emissions generally.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Ehn, Mikael -- Thornton, Joel A -- Kleist, Einhard -- Sipila, Mikko -- Junninen, Heikki -- Pullinen, Iida -- Springer, Monika -- Rubach, Florian -- Tillmann, Ralf -- Lee, Ben -- Lopez-Hilfiker, Felipe -- Andres, Stefanie -- Acir, Ismail-Hakki -- Rissanen, Matti -- Jokinen, Tuija -- Schobesberger, Siegfried -- Kangasluoma, Juha -- Kontkanen, Jenni -- Nieminen, Tuomo -- Kurten, Theo -- Nielsen, Lasse B -- Jorgensen, Solvejg -- Kjaergaard, Henrik G -- Canagaratna, Manjula -- Maso, Miikka Dal -- Berndt, Torsten -- Petaja, Tuukka -- Wahner, Andreas -- Kerminen, Veli-Matti -- Kulmala, Markku -- Worsnop, Douglas R -- Wildt, Jurgen -- Mentel, Thomas F -- England -- Nature. 2014 Feb 27;506(7489):476-9. doi: 10.1038/nature13032.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉1] Institute for Energy and Climate Research (IEK-8), Forschungszentrum Julich, 52425 Julich, Germany [2] Department of Physics, PO Box 64, 00014 University of Helsinki, Finland. ; 1] Department of Physics, PO Box 64, 00014 University of Helsinki, Finland [2] Department of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, USA. ; Institute of Bio- and Geosciences (IBG-2), Forschungszentrum Julich, 52425 Julich, Germany. ; Department of Physics, PO Box 64, 00014 University of Helsinki, Finland. ; Institute for Energy and Climate Research (IEK-8), Forschungszentrum Julich, 52425 Julich, Germany. ; Department of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, USA. ; 1] Department of Physics, PO Box 64, 00014 University of Helsinki, Finland [2] Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany. ; 1] Department of Physics, PO Box 64, 00014 University of Helsinki, Finland [2] Helsinki Institute of Physics, PO Box 64, 00014 University of Helsinki, Finland. ; Department of Chemistry, PO Box 55, 00014 University of Helsinki, Finland. ; Department of Chemistry, University of Copenhagen, Universitetsparken 5, 2100 Copenhagen O, Denmark. ; Aerodyne Research, Inc., 45 Manning Road, Billerica, Massachusetts 01821, USA. ; Department of Physics, Tampere University of Technology, PO Box 692, 33101 Tampere, Finland. ; Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany. ; 1] Department of Physics, PO Box 64, 00014 University of Helsinki, Finland [2] Aerodyne Research, Inc., 45 Manning Road, Billerica, Massachusetts 01821, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24572423" target="_blank"〉PubMed〈/a〉
    Keywords: Aerosols/analysis/*chemistry/metabolism ; Atmosphere/chemistry ; Climate ; Ecosystem ; Finland ; Gases/analysis/chemistry ; *Models, Chemical ; Monoterpenes/chemistry ; Oxidation-Reduction ; Ozone/chemistry ; Particle Size ; Trees/metabolism ; Volatile Organic Compounds/analysis/*chemistry/metabolism ; Volatilization
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2013-08-31
    Description: During the Airborne Antarctic Ozone Experiment from 28 August to 30 September 1987 near UV zenith scattered sky measurements were made over Antarctic from the NASA DC-8 aircraft using a one third m spectrograph equipped with a diode-array detector. Scattered sky light data in the wavelength range 348 nm to 388 nm was spectrally analyzed for O3, NO2, OClO, and BrO column abundances. Slant column abudances of O3, NO2, OClO and BrO were determined, using a computer algorithm of non-linear and linear least square correlation of Antarctic scattered sky spectra to laboratory absorption cross section data. Using measured vertical electrochemical sonde ozone profiles from Palmer, Halley Bay, and the South Pole Stations the slant columns of O3 were converted into vertical column abundances. The vertical column amounts of NO2, OClO, and BrO were derived using vertical profiles calculated by a chemical model appropriate for Antarctica. NO2 vertical column abundances show steep latitudinal decrease with increasing latitude for all 13 flights carried out during the mission. In the regions where NO2 abudances are low, OClO and BrO were observed. The spatial and temporal vertical column abundances of these species are discussed in the context of the chemistry and dynamics in the antarctic polar vortex during the austral spring.
    Keywords: ENVIRONMENT POLLUTION
    Type: NASA, Goddard Space Flight Center, Polar Ozone Workshop. Abstracts; p 119
    Format: application/pdf
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