Controls on the tropospheric oxidizing capacity during an idealized Dansgaard-Oeschger event, and their implications for the rapid rises in atmospheric methane during the last glacial period
about
Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records.Atmospheric methane variability: Centennial-scale signals in the Last Glacial PeriodCarbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2
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Controls on the tropospheric oxidizing capacity during an idealized Dansgaard-Oeschger event, and their implications for the rapid rises in atmospheric methane during the last glacial period
description
im Juni 2012 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована в червні 2012
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Controls on the tropospheric o ...... during the last glacial period
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Controls on the tropospheric o ...... during the last glacial period
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Controls on the tropospheric o ...... during the last glacial period
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Controls on the tropospheric o ...... during the last glacial period
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Controls on the tropospheric o ...... during the last glacial period
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Controls on the tropospheric o ...... during the last glacial period
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Controls on the tropospheric o ...... during the last glacial period
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E. W. Wolff
J. G. Levine
P. J. Valdes
P. O. Hopcroft
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P356
10.1029/2012GL051866
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P577
2012-06-28T00:00:00Z