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Large stocks of peatland carbon and nitrogen are vulnerable to permafrost thaw

Hugelius, Gustaf (author)
Stockholms universitet,Institutionen för naturgeografi,Stanford University, USA
Loisel, Julie (author)
Chadburn, Sarah (author)
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Jackson, Robert B. (author)
Jones, Miriam (author)
MacDonald, Glen (author)
Marushchak, Maija (author)
Olefeldt, David (author)
Packalen, Maara (author)
Siewert, Matthias B. (author)
Umeå universitet,Institutionen för ekologi, miljö och geovetenskap,Arcum
Treat, Claire (author)
Turetsky, Merritt (author)
Voigt, Carolina (author)
Yu, Zicheng (author)
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 (creator_code:org_t)
2020-08-10
2020
English.
In: Proceedings of the National Academy of Sciences of the United States of America. - : Proceedings of the National Academy of Sciences. - 0027-8424 .- 1091-6490. ; 117:34, s. 20438-20446
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Northern peatlands have accumulated large stocks of organic carbon (C) and nitrogen (N), but their spatial distribution and vulnerability to climate warming remain uncertain. Here, we used machine-learning techniques with extensive peat core data (n > 7,000) to create observation-based maps of northern peatland C and N stocks, and to assess their response to warming and permafrost thaw. We estimate that northern peatlands cover 3.7 ± 0.5 million km2 and store 415 ± 150 Pg C and 10 ± 7 Pg N. Nearly half of the peatland area and peat C stocks are permafrost affected. Using modeled global warming stabilization scenarios (from 1.5 to 6 °C warming), we project that the current sink of atmospheric C (0.10 ± 0.02 Pg C⋅y−1) in northern peatlands will shift to a C source as 0.8 to 1.9 million km2 of permafrost-affected peatlands thaw. The projected thaw would cause peatland greenhouse gas emissions equal to ∼1% of anthropogenic radiative forcing in this century. The main forcing is from methane emissions (0.7 to 3 Pg cumulative CH4-C) with smaller carbon dioxide forcing (1 to 2 Pg CO2-C) and minor nitrous oxide losses. We project that initial CO2-C losses reverse after ∼200 y, as warming strengthens peatland C-sinks. We project substantial, but highly uncertain, additional losses of peat into fluvial systems of 10 to 30 Pg C and 0.4 to 0.9 Pg N. The combined gaseous and fluvial peatland C loss estimated here adds 30 to 50% onto previous estimates of permafrost-thaw C losses, with southern permafrost regions being the most vulnerable.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)

Keyword

northern peatlands
carbon stocks
nitrogen stocks
greenhouse gas fluxes
permafrost thaw

Publication and Content Type

ref (subject category)
art (subject category)

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