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Carbon dioxide release from retrogressive thaw slumps in Siberia

Thawing of ice-rich permafrost soils in sloped terrain can lead to activation of retrogressive thaw slumps (RTSs) which make organic matter available for decomposition that has been frozen for centuries to millennia. Recent studies show that the area affected by RTSs increased in the last two decade...

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Auteurs principaux: C Beer, A Runge, G Grosse, G Hugelius, C Knoblauch
Format: Artigo
Langue:Inglês
Publié: IOP Publishing 2023-01-01
Collection:Environmental Research Letters
Sujets:
Accès en ligne:https://doi.org/10.1088/1748-9326/acfdbb
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