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  • American Association for the Advancement of Science (AAAS)  (3)
  • 1
    Publication Date: 2009-01-24
    Description: Carbonaceous aerosols cause strong atmospheric heating and large surface cooling that is as important to South Asian climate forcing as greenhouse gases, yet the aerosol sources are poorly understood. Emission inventory models suggest that biofuel burning accounts for 50 to 90% of emissions, whereas the elemental composition of ambient aerosols points to fossil fuel combustion. We used radiocarbon measurements of winter monsoon aerosols from western India and the Indian Ocean to determine that biomass combustion produced two-thirds of the bulk carbonaceous aerosols, as well as one-half and two-thirds of two black carbon subfractions, respectively. These constraints show that both biomass combustion (such as residential cooking and agricultural burning) and fossil fuel combustion should be targeted to mitigate climate effects and improve air quality.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Gustafsson, Orjan -- Krusa, Martin -- Zencak, Zdenek -- Sheesley, Rebecca J -- Granat, Lennart -- Engstrom, Erik -- Praveen, P S -- Rao, P S P -- Leck, Caroline -- Rodhe, Henning -- New York, N.Y. -- Science. 2009 Jan 23;323(5913):495-8. doi: 10.1126/science.1164857.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Applied Environmental Science, Stockholm University, 10691 Stockholm, Sweden. orjan.gustafsson@itm.su.se〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19164746" 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: 2010-03-06
    Description: Remobilization to the atmosphere of only a small fraction of the methane held in East Siberian Arctic Shelf (ESAS) sediments could trigger abrupt climate warming, yet it is believed that sub-sea permafrost acts as a lid to keep this shallow methane reservoir in place. Here, we show that more than 5000 at-sea observations of dissolved methane demonstrates that greater than 80% of ESAS bottom waters and greater than 50% of surface waters are supersaturated with methane regarding to the atmosphere. The current atmospheric venting flux, which is composed of a diffusive component and a gradual ebullition component, is on par with previous estimates of methane venting from the entire World Ocean. Leakage of methane through shallow ESAS waters needs to be considered in interactions between the biogeosphere and a warming Arctic climate.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Shakhova, Natalia -- Semiletov, Igor -- Salyuk, Anatoly -- Yusupov, Vladimir -- Kosmach, Denis -- Gustafsson, Orjan -- New York, N.Y. -- Science. 2010 Mar 5;327(5970):1246-50. doi: 10.1126/science.1182221.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉International Arctic Research Centre, University of Alaska, Fairbanks, AK 99709, USA. nshakhov@iarc.uaf.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20203047" 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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  • 3
    Publication Date: 2019
    Description: 〈p〉Light-absorbing organic aerosols, known as brown carbon (BrC), counteract the overall cooling effect of aerosols on Earth’s climate. The spatial and temporal dynamics of their light-absorbing properties are poorly constrained and unaccounted for in climate models, because of limited ambient observations. We combine carbon isotope forensics (〈sup〉13〈/sup〉C) with measurements of light absorption in a conceptual aging model to constrain the loss of light absorptivity (i.e., bleaching) of water-soluble BrC (WS-BrC) aerosols in one of the world’s largest BrC emission regions—South Asia. On this regional scale, we find that atmospheric photochemical oxidation reduces the light absorption of WS-BrC by ~84% during transport over 6000 km in the Indo-Gangetic Plain, with an ambient first-order bleaching rate of 0.20 ± 0.05 day〈sup〉–1〈/sup〉 during over-ocean transit across Bay of Bengal to an Indian Ocean receptor site. This study facilitates dynamic parameterization of WS-BrC absorption properties, thereby constraining BrC climate impact over South Asia.〈/p〉
    Electronic ISSN: 2375-2548
    Topics: Natural Sciences in General
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