Marcin Jackowicz-Korczynski
Forskningsingenjör
Increased nitrous oxide emissions from Arctic peatlands after permafrost thaw
Författare
Summary, in English
Permafrost in the Arctic is thawing, exposing large carbon and nitrogen stocks for decomposition. Gaseous carbon release from Arctic soils due to permafrost thawing is known to be substantial, but growing evidence suggests that Arctic soils may also be relevant sources of nitrous oxide (N2O). Here we show that N2O emissions from subarctic peatlands increase as the permafrost thaws. In our study, the highest postthaw emissions occurred from bare peat surfaces, a typical landform in permafrost peatlands, where permafrost thaw caused a fivefold increase in emissions (0.56 ± 0.11 vs. 2.81 ± 0.6 mg N2O m-2 d-1). These emission rates match those from tropical forest soils, the world's largest natural terrestrial N2O source. The presence of vegetation, known to limit N2O emissions in tundra, did decrease (by ∼90%) but did not prevent thaw-induced N2O release, whereas waterlogged conditions suppressed the emissions. We show that regions with high probability for N2O emissions cover one-fourth of the Arctic. Our results imply that the Arctic N2O budget will depend strongly on moisture changes, and that a gradual deepening of the active layer will create a strong noncarbon climate change feedback.
Avdelning/ar
- Institutionen för naturgeografi och ekosystemvetenskap
- MERGE: ModElling the Regional and Global Earth system
- BECC: Biodiversity and Ecosystem services in a Changing Climate
Publiceringsår
2017-06-13
Språk
Engelska
Sidor
6238-6243
Publikation/Tidskrift/Serie
Proceedings of the National Academy of Sciences of the United States of America
Volym
114
Issue
24
Dokumenttyp
Artikel i tidskrift
Förlag
National Academy of Sciences
Ämne
- Climate Research
- Meteorology and Atmospheric Sciences
Nyckelord
- Arctic soils
- Climate change
- Greenhouse gases
- Nitrogen
- Tundra
Aktiv
Published
ISBN/ISSN/Övrigt
- ISSN: 0027-8424