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• W2099688870 abstract "Abstract. Boreal regions comprise about 17 % of the global land area, and they both affect and are influenced by climate change. To better understand boreal forest fire emissions and plume evolution, 947 whole air samples were collected aboard the NASA DC-8 research aircraft in summer 2008 as part of the ARCTAS-B field mission, and analyzed for 79 non-methane volatile organic compounds (NMVOCs) using gas chromatography. Together with simultaneous measurements of CO2, CO, CH4, CH2O, NO2, NO, HCN and CH3CN, these measurements represent the most comprehensive assessment of trace gas emissions from boreal forest fires to date. Based on 105 air samples collected in fresh Canadian smoke plumes, 57 of the 80 measured NMVOCs (including CH2O) were emitted from the fires, including 45 species that were quantified from boreal forest fires for the first time. After CO2, CO and CH4, the largest emission factors (EFs) for individual species were formaldehyde (2.1 ± 0.2 g kg−1), followed by methanol, NO2, HCN, ethene, α-pinene, β-pinene, ethane, benzene, propene, acetone and CH3CN. Globally, we estimate that boreal forest fires release 2.4 ± 0.6 Tg C yr−1 in the form of NMVOCs, with approximately 41 % of the carbon released as C1-C2 NMVOCs and 21 % as pinenes. These are the first reported field measurements of monoterpene emissions from boreal forest fires, and we speculate that the pinenes, which are relatively heavy molecules, were detected in the fire plumes as the result of distillation of stored terpenes as the vegetation is heated. Their inclusion in smoke chemistry models is expected to improve model predictions of secondary organic aerosol (SOA) formation. The fire-averaged EF of dichloromethane or CH2Cl2, (6.9 ± 8.6) × 10−4 g kg−1, was not significantly different from zero and supports recent findings that its global biomass burning source appears to have been overestimated. Similarly, we found no evidence for emissions of chloroform (CHCl3) or methyl chloroform (CH3CCl3) from boreal forest fires. The speciated hydrocarbon measurements presented here show the importance of carbon released by short-chain NMVOCs, the strong contribution of pinene emissions from boreal forest fires, and the wide range of compound classes in the most abundantly emitted NMVOCs, all of which can be used to improve biomass burning inventories in local/global models and reduce uncertainties in model estimates of trace gas emissions and their impact on the atmosphere." @default.
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• W2099688870 date "2011-07-07" @default.
• W2099688870 modified "2023-10-05" @default.
• W2099688870 title "Boreal forest fire emissions in fresh Canadian smoke plumes: C&lt;sub&gt;1&lt;/sub&gt;-C&lt;sub&gt;10&lt;/sub&gt; volatile organic compounds (VOCs), CO&lt;sub&gt;2&lt;/sub&gt;, CO, NO&lt;sub&gt;2&lt;/sub&gt;, NO, HCN and CH&lt;sub&gt;3&lt;/sub&gt;CN" @default.
• W2099688870 cites W1491887116 @default.
• W2099688870 cites W1563424411 @default.
• W2099688870 cites W1600578893 @default.
• W2099688870 cites W1899662808 @default.
• W2099688870 cites W1964252479 @default.
• W2099688870 cites W1964572794 @default.
• W2099688870 cites W1970391023 @default.
• W2099688870 cites W1976393863 @default.
• W2099688870 cites W1979045233 @default.
• W2099688870 cites W1983346223 @default.
• W2099688870 cites W1984321597 @default.
• W2099688870 cites W1988060312 @default.
• W2099688870 cites W1988597968 @default.
• W2099688870 cites W1989364707 @default.
• W2099688870 cites W1989438093 @default.
• W2099688870 cites W1998277551 @default.
• W2099688870 cites W1999882196 @default.
• W2099688870 cites W2001177666 @default.
• W2099688870 cites W2003760553 @default.
• W2099688870 cites W2012349632 @default.
• W2099688870 cites W2013525488 @default.
• W2099688870 cites W2024791433 @default.
• W2099688870 cites W2026354693 @default.
• W2099688870 cites W2039720350 @default.
• W2099688870 cites W2044382784 @default.
• W2099688870 cites W2044499383 @default.
• W2099688870 cites W2044547052 @default.
• W2099688870 cites W2045398695 @default.
• W2099688870 cites W2050771205 @default.
• W2099688870 cites W2050809573 @default.
• W2099688870 cites W2051755599 @default.
• W2099688870 cites W2052953021 @default.
• W2099688870 cites W2064348969 @default.
• W2099688870 cites W2065898001 @default.
• W2099688870 cites W2069595208 @default.
• W2099688870 cites W2071563634 @default.
• W2099688870 cites W2071706389 @default.
• W2099688870 cites W2079055208 @default.
• W2099688870 cites W2085685120 @default.
• W2099688870 cites W2086500762 @default.
• W2099688870 cites W2096156479 @default.
• W2099688870 cites W2101845599 @default.
• W2099688870 cites W2101956016 @default.
• W2099688870 cites W2104837514 @default.
• W2099688870 cites W2106063030 @default.
• W2099688870 cites W2106636153 @default.
• W2099688870 cites W2111155943 @default.
• W2099688870 cites W2113649743 @default.
• W2099688870 cites W2115450031 @default.
• W2099688870 cites W2123929265 @default.
• W2099688870 cites W2124904730 @default.
• W2099688870 cites W2134844911 @default.
• W2099688870 cites W2134927874 @default.
• W2099688870 cites W2136814444 @default.
• W2099688870 cites W2139686657 @default.
• W2099688870 cites W2144304061 @default.
• W2099688870 cites W2145117854 @default.
• W2099688870 cites W2149390613 @default.
• W2099688870 cites W2149814081 @default.
• W2099688870 cites W2149825932 @default.
• W2099688870 cites W2152410413 @default.
• W2099688870 cites W2156291370 @default.
• W2099688870 cites W2156632972 @default.
• W2099688870 cites W2157769063 @default.
• W2099688870 cites W2158091070 @default.
• W2099688870 cites W2163972700 @default.
• W2099688870 cites W2168101315 @default.
• W2099688870 cites W2169477247 @default.
• W2099688870 cites W2170531874 @default.
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• W2099688870 doi "https://doi.org/10.5194/acp-11-6445-2011" @default.
• W2099688870 hasPublicationYear "2011" @default.
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