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Effects of experimental warming of air, soil and permafrost on carbon balance in Alaskan tundraAuthor(s): S.M. Natali; E.A.G. Schuur; C. Trucco; C.E. Hicks Pries; K.G. Crummer; A.F. Baron Lopez
Source: Global Change Biology. 17(3): 1394-1407
Publication Series: Scientific Journal (JRNL)
Station: Pacific Northwest Research Station
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DescriptionThe carbon (C) storage capacity of northern latitude ecosystems may diminish as warming air temperatures increase permafrost thaw and stimulate decomposition of previously frozen soil organic C. However, warming may also enhance plant growth so that photosynthetic carbon dioxide (C02) uptake may, in part, offset respiratory losses. To determine the effects of air and soil warming on C02 exchange in tundra, we established an ecosystem warming experiment—the Carbon in Permafrost Experimental Heating Research (CiPEHR) project—in the northern foothills of the Alaska Range in Interior Alaska. We used snow fences coupled with spring snow removal to increase deep soil temperatures and thaw depth (winter warming) and open-top chambers to increase growing season air temperatures (summer warming). While most changes to the abiotic environment at CiPEHR were driven by winter warming, summer warming effects on plant and soil processes resulted in 20% increases in both gross primary productivity and growing season ecosystem respiration and significantly altered the age and sources of C02 respired from this ecosystem. These results demonstrate the vulnerability of organic C stored in near surface permafrost to increasing temperatures and the strong potential for warming tundra to serve as a positive feedback to global climate change.
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CitationNatali, Susan M.; Schuur, Edward A.G.; Trucco, Christian; Hicks Pries, Caitlin E.; Crummer, Kathryn G.; Baron Lopez, Andres F. 2011. Effects of experimental warming of air, soil and permafrost on carbon balance in Alaskan tundra. Global Change Biology. 17(3): 1394-1407.
Keywordsclimate change, NEE, permafrost, radiocarbon, snowfence, soil carbon, thermokarst, tundra, warming
- Increased plant productivity in Alaskan tundra as a result of experimental warming of soil and permafrost
- Permafrost degradation stimulates carbon loss from experimentally warmed tundra
- Soil CO2 production in upland tundra where permafrost is thawing
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