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Isotopic seasonality of fluvial-derived greenhouse gases implies active layer deepening

Climate change in the northern circumpolar regions is rapidly thawing organic-rich permafrost soils, leading to the substantial release of dissolved CO _2 and CH _4 into river systems. This mobilization impacts local ecosystems and regional climate feedback loops, playing a crucial role in the Arcti...

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Auteurs principaux: Melissa S Schwab, Clayton D Elder, Xiaomei Xu, Claudia I Czimczik, Charles E Miller
Format: Artigo
Langue:Inglês
Publié: IOP Publishing 2024-01-01
Collection:Environmental Research Letters
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Accès en ligne:https://doi.org/10.1088/1748-9326/ad820f
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