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  • 1
    Publication Date: 2012-09-01
    Description: The fine particles serving as cloud condensation nuclei in pristine Amazonian rainforest air consist mostly of secondary organic aerosol. Their origin is enigmatic, however, because new particle formation in the atmosphere is not observed. Here, we show that the growth of organic aerosol particles can be initiated by potassium-salt-rich particles emitted by biota in the rainforest. These particles act as seeds for the condensation of low- or semi-volatile organic compounds from the atmospheric gas phase or multiphase oxidation of isoprene and terpenes. Our findings suggest that the primary emission of biogenic salt particles directly influences the number concentration of cloud condensation nuclei and affects the microphysics of cloud formation and precipitation over the rainforest.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Pohlker, Christopher -- Wiedemann, Kenia T -- Sinha, Barbel -- Shiraiwa, Manabu -- Gunthe, Sachin S -- Smith, Mackenzie -- Su, Hang -- Artaxo, Paulo -- Chen, Qi -- Cheng, Yafang -- Elbert, Wolfgang -- Gilles, Mary K -- Kilcoyne, Arthur L D -- Moffet, Ryan C -- Weigand, Markus -- Martin, Scot T -- Poschl, Ulrich -- Andreae, Meinrat O -- New York, N.Y. -- Science. 2012 Aug 31;337(6098):1075-8. doi: 10.1126/science.1223264.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Biogeochemistry Department, Max Planck Institute for Chemistry, Mainz 55020, Germany. c.pohlker@mpic.de〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22936773" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/*chemistry ; Particle Size ; Particulate Matter/*chemistry ; Potassium/*chemistry ; Rain/*chemistry ; Salts/chemistry ; South America ; Trees/*chemistry
    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: 2013-05-11
    Description: Global sulfate production plays a key role in aerosol radiative forcing; more than half of this production occurs in clouds. We found that sulfur dioxide oxidation catalyzed by natural transition metal ions is the dominant in-cloud oxidation pathway. The pathway was observed to occur primarily on coarse mineral dust, so the sulfate produced will have a short lifetime and little direct or indirect climatic effect. Taking this into account will lead to large changes in estimates of the magnitude and spatial distribution of aerosol forcing. Therefore, this oxidation pathway-which is currently included in only one of the 12 major global climate models-will have a significant impact on assessments of current and future climate.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Harris, Eliza -- Sinha, Barbel -- van Pinxteren, Dominik -- Tilgner, Andreas -- Fomba, Khanneh Wadinga -- Schneider, Johannes -- Roth, Anja -- Gnauk, Thomas -- Fahlbusch, Benjamin -- Mertes, Stephan -- Lee, Taehyoung -- Collett, Jeffrey -- Foley, Stephen -- Borrmann, Stephan -- Hoppe, Peter -- Herrmann, Hartmut -- New York, N.Y. -- Science. 2013 May 10;340(6133):727-30. doi: 10.1126/science.1230911.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Particle Chemistry Department, Max Planck Institute for Chemistry, Mainz, Germany. elizah@mit.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23661757" target="_blank"〉PubMed〈/a〉
    Keywords: Aerosols ; Atmosphere/*chemistry ; Catalysis ; *Climate ; *Dust ; Minerals/chemistry ; Oxidation-Reduction ; Sulfur Dioxide/*chemistry ; Transition Elements
    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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