Tundra Underlain By Thawing Permafrost Persistently Emits Carbon to the Atmosphere Over 15 Years of Measurements

• Main Authors: Schuur, Edward AG, Bracho, Rosvel, Celis, Gerardo, Belshe, E Fay, Ebert, Chris, Ledman, Justin, Mauritz, Marguerite, Pegoraro, Elaine F, Plaza, César, Rodenhizer, Heidi, Romanovsky, Vladimir, Schädel, Christina, Schirokauer, David, Taylor, Meghan, Vogel, Jason G, Webb, Elizabeth E
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: eScholarship, University of California 2021
• Subjects: Climate Action; Arctic; carbon; eddy covariance; permafrost; tundra; Geophysics; Climate change; Tundra; Alaska
• Online Access: https://escholarship.org/uc/item/7vc4s2hf

Warming of the Arctic can stimulate microbial decomposition and release of permafrost soil carbon (C) as greenhouse gases, and thus has the potential to influence climate change. At the same time, plant growth can be stimulated and offset C release. This study presents a 15-year time series comprising chamber and eddy covariance measurements of net ecosystem C exchange in a tundra ecosystem in Alaska where permafrost has been degrading due to regional warming. The site was a carbon dioxide source to the atmosphere with a cumulative total loss of 781.6g C m−2 over the study period. Both gross primary productivity (GPP) and ecosystem respiration (Reco) were already likely higher than historical levels such that increases in Reco losses overwhelmed GPP gains in most years. This shift to a net C source to the atmosphere likely started in the early 1990s when permafrost was observed to warm and thaw at the site. Shifts in the plant community occur more slowly and are likely to constrain future GPP increases as compared to more rapid shifts in the microbial community that contribute to increased Reco. Observed rates suggest that cumulative net soil C loss of 4.18–10.00kg C m−2—8%–20% of the current active layer soil C pool—could occur from 2020 to the end of the century. This amount of permafrost C loss to the atmosphere represents a significant accelerating feedback to climate change if it were to occur at a similar magnitude across the permafrost region.