A 21st-century shift from fossil-fuel to biogenic methane emissions indicated by 13CH4.

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Bibliographic Details
Title: A 21st-century shift from fossil-fuel to biogenic methane emissions indicated by 13CH4.
Authors: Schaefer, Hinrich, Fletcher, Sara E. Mikaloff, Veidt, Cordelia, Lassey, Keith R., Brailsford, Gordon W., Bromley, Tony M., Dlugokencky, Edward J., Michel, Sylvia E., Miller, John B., Levin, Ingeborg, Lowe, Dave C., Martin, Ross J., Vaughn, Bruce H., White, James W. C.
Source: Science (pre-March 2025). 4/1/2016, Vol. 352 Issue 6281, p80-84. 5p.
Subjects: Atmospheric methane, Atmospheric chemistry, Fossil fuels, Emissions (Air pollution), Air pollution
Abstract: 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. [ABSTRACT FROM AUTHOR]
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Database: Psychology and Behavioral Sciences Collection
Description
Abstract: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. [ABSTRACT FROM AUTHOR]
ISSN:00368075
DOI:10.1126/science.aad2705