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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| Autors principals: | , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
IOP Publishing
2024-01-01
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| Col·lecció: | Environmental Research Letters |
| Matèries: | |
| Accés en línia: | https://doi.org/10.1088/1748-9326/ad820f |
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