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• W2034797404 abstract "Research Article| June 01, 2013 Combined bromine and chlorine release from large explosive volcanic eruptions: A threat to stratospheric ozone? S. Kutterolf; S. Kutterolf * 1GEOMAR Helmholtz Centre for Ocean Research, SFB574, Wischhofstrasse 1-3, 24148 Kiel, Germany *E-mail: skutterolf@geomar.de. Search for other works by this author on: GSW Google Scholar T.H. Hansteen; T.H. Hansteen 1GEOMAR Helmholtz Centre for Ocean Research, SFB574, Wischhofstrasse 1-3, 24148 Kiel, Germany Search for other works by this author on: GSW Google Scholar K. Appel; K. Appel 2HASYLAB at DESY, Notkestrasse 85, 22607 Hamburg, Germany Search for other works by this author on: GSW Google Scholar A. Freundt; A. Freundt 1GEOMAR Helmholtz Centre for Ocean Research, SFB574, Wischhofstrasse 1-3, 24148 Kiel, Germany Search for other works by this author on: GSW Google Scholar K. Krüger; K. Krüger 1GEOMAR Helmholtz Centre for Ocean Research, SFB574, Wischhofstrasse 1-3, 24148 Kiel, Germany Search for other works by this author on: GSW Google Scholar W. Pérez; W. Pérez 1GEOMAR Helmholtz Centre for Ocean Research, SFB574, Wischhofstrasse 1-3, 24148 Kiel, Germany Search for other works by this author on: GSW Google Scholar H. Wehrmann H. Wehrmann 1GEOMAR Helmholtz Centre for Ocean Research, SFB574, Wischhofstrasse 1-3, 24148 Kiel, Germany Search for other works by this author on: GSW Google Scholar Author and Article Information S. Kutterolf * 1GEOMAR Helmholtz Centre for Ocean Research, SFB574, Wischhofstrasse 1-3, 24148 Kiel, Germany T.H. Hansteen 1GEOMAR Helmholtz Centre for Ocean Research, SFB574, Wischhofstrasse 1-3, 24148 Kiel, Germany K. Appel 2HASYLAB at DESY, Notkestrasse 85, 22607 Hamburg, Germany A. Freundt 1GEOMAR Helmholtz Centre for Ocean Research, SFB574, Wischhofstrasse 1-3, 24148 Kiel, Germany K. Krüger 1GEOMAR Helmholtz Centre for Ocean Research, SFB574, Wischhofstrasse 1-3, 24148 Kiel, Germany W. Pérez 1GEOMAR Helmholtz Centre for Ocean Research, SFB574, Wischhofstrasse 1-3, 24148 Kiel, Germany H. Wehrmann 1GEOMAR Helmholtz Centre for Ocean Research, SFB574, Wischhofstrasse 1-3, 24148 Kiel, Germany *E-mail: skutterolf@geomar.de. Publisher: Geological Society of America Received: 14 Sep 2012 Revision Received: 25 Jan 2013 Accepted: 30 Jan 2013 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2013 Geological Society of America Geology (2013) 41 (6): 707–710. https://doi.org/10.1130/G34044.1 Article history Received: 14 Sep 2012 Revision Received: 25 Jan 2013 Accepted: 30 Jan 2013 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation S. Kutterolf, T.H. Hansteen, K. Appel, A. Freundt, K. Krüger, W. Pérez, H. Wehrmann; Combined bromine and chlorine release from large explosive volcanic eruptions: A threat to stratospheric ozone?. Geology 2013;; 41 (6): 707–710. doi: https://doi.org/10.1130/G34044.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Large explosive volcanic eruptions inject gases, aerosols, and fine ashes into the stratosphere, potentially influencing climate. Emissions of chlorine (Cl) and bromine (Br) from such large eruptions play an important role for catalytic destruction of ozone in the stratosphere, but hitherto the global effects of simultaneous catastrophic release of volcanic Br and Cl into the stratosphere have not been investigated. The Br release from 14 large explosive eruptions throughout Nicaragua covering an entire subduction zone segment in the past 70 ka was determined with petrologic methods. Melt inclusions in volcanic phenocrysts were analyzed using a new optimized synchrotron–X-ray fluorescence microprobe set-up. Single eruptions produced Br outputs of 4–600 kt, giving an average Br emission of 27 kt per eruption. Using the assumption that 10% of the emitted halogens reach the stratosphere, the average Br and Cl loading to the stratosphere would be 3 ppt and 1500 ppt, respectively, which together would account for 185% of the preindustrial equivalent effective stratospheric Cl loading. We thus conclude that many large tropical volcanic eruptions had and have the potential to substantially deplete ozone on a global scale, eventually forming future ozone holes. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2034797404 title "Combined bromine and chlorine release from large explosive volcanic eruptions: A threat to stratospheric ozone?" @default.
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