2021
DOI: 10.1073/pnas.2107632118
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Methane release from carbonate rock formations in the Siberian permafrost area during and after the 2020 heat wave

Abstract: Anthropogenic global warming may be accelerated by a positive feedback from the mobilization of methane from thawing Arctic permafrost. There are large uncertainties about the size of carbon stocks and the magnitude of possible methane emissions. Methane cannot only be produced from the microbial decay of organic matter within the thawing permafrost soils (microbial methane) but can also come from natural gas (thermogenic methane) trapped under or within the permafrost layer and released when it thaws. In the … Show more

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Cited by 34 publications
(23 citation statements)
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“…For example, fires in the Arctic circle deposit soot on the ice, meaning it absorbs more sunlight, heating it up and causing more to melt [9]. The permafrost is also melting, releasing tonnes of methane [10] e a greenhouse gas that is 25 times more effective than carbon dioxide e causing more heating. At the same time, the species extinction rate is between 100 and 1000 times background [11], and we know that biodiversity is essential to support our agricultural systems.…”
mentioning
confidence: 99%
“…For example, fires in the Arctic circle deposit soot on the ice, meaning it absorbs more sunlight, heating it up and causing more to melt [9]. The permafrost is also melting, releasing tonnes of methane [10] e a greenhouse gas that is 25 times more effective than carbon dioxide e causing more heating. At the same time, the species extinction rate is between 100 and 1000 times background [11], and we know that biodiversity is essential to support our agricultural systems.…”
mentioning
confidence: 99%
“…16). Such features can be easily misinterpreted as a local methane emission signal (see Froitzheim et al, 2021).…”
Section: Sentinel-5 Precursor Operational Xch 4 Productmentioning
confidence: 99%
“…Or take the example of methane, a potent if shorter lived greenhouse gas (Fewster et al 2022). The already ongoing methane releases from thawing permafrost regions (Hugelius et al 2020) and the sea floor (Froitzheim et al 2021) contribute to the warming of the Arctic. This will probably trigger additional massive releases of methane from biomass and geological deposits once the loss of permafrost enabling temperatures across almost all of the Eurasian Arctic materialises, which is expected to happen before 2040.…”
Section: The Anthropocene-a New Geological Agementioning
confidence: 99%