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DOI | 10.1126/science.aad2705 |
A 21st-century shift from fossil-fuel to biogenic methane emissions indicated by 13CH4 | |
Schaefer H.; Fletcher S.E.M.; Veidt C.; Lassey K.R.; Brailsford G.W.; Bromley T.M.; Dlugokencky E.J.; Michel S.E.; Miller J.B.; Levin I.; Lowe D.C.; Martin R.J.; Vaughn B.H.; White J.W.C. | |
发表日期 | 2016 |
ISSN | 0036-8075 |
起始页码 | 80 |
结束页码 | 84 |
卷号 | 352期号:6281 |
英文摘要 | Between 1999 and 2006, a plateau interrupted the otherwise continuous increase of atmospheric methane concentration [CH4] since preindustrial times. Causes could be sink variability or a temporary reduction in industrial or climate-sensitive sources. We reconstructed the global history of [CH4] and its stable carbon isotopes from ice cores, archived air, and a global network of monitoring stations. A box-model analysis suggests that diminishing thermogenic emissions, probably from the fossil-fuel industry, and/or variations in the hydroxyl CH4 sink caused the [CH4] plateau. Thermogenic emissions did not resume to cause the renewed [CH4] rise after 2006, which contradicts emission inventories. Post-2006 source increases are predominantly biogenic, outside the Arctic, and arguably more consistent with agriculture than wetlands. If so, mitigating CH4 emissions must be balanced with the need for food production. |
英文关键词 | carbon; coal; fossil fuel; methane; natural gas; ozone; atmospheric dynamics; biogenic emission; concentration (composition); emission inventory; fossil fuel; methane; reconstruction; spatiotemporal analysis; stable isotope; boundary layer; carbon footprint; carbon source; climate change; environmental change; food industry; human; human activities; nonhuman; priority journal; remote sensing; Review; thermogenesis; troposphere; water vapor; wetland; Arctic |
语种 | 英语 |
来源期刊 | Science
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/245350 |
作者单位 | Climate and Atmosphere Center, National Institute of Water and Atmospheric Research (NIWA), 301 Evans Bay Parade, Wellington, 6021, New Zealand; Institut für Umweltphysik, Heidelberg University, Im Neuenheimer Feld 229, Heidelberg, 69120, Germany; National Oceanic and Atmospheric Administration (NOAA), Earth System Research Laboratory (ESRL), Global Monitoring Division, 325 Broadway, Boulder, CO 80305, United States; Institute of Arctic and Alpine Research (INSTAAR), University of Colorado, Boulder, CO 80309, United States; Lassey Research and Education, 4 Witako Street, Lower Hutt, 5011, New Zealand; LoweNZ, 31 Queen Street, Lower Hutt, 5012, New Zealand |
推荐引用方式 GB/T 7714 | Schaefer H.,Fletcher S.E.M.,Veidt C.,et al. A 21st-century shift from fossil-fuel to biogenic methane emissions indicated by 13CH4[J],2016,352(6281). |
APA | Schaefer H..,Fletcher S.E.M..,Veidt C..,Lassey K.R..,Brailsford G.W..,...&White J.W.C..(2016).A 21st-century shift from fossil-fuel to biogenic methane emissions indicated by 13CH4.Science,352(6281). |
MLA | Schaefer H.,et al."A 21st-century shift from fossil-fuel to biogenic methane emissions indicated by 13CH4".Science 352.6281(2016). |
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