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Biomass offsets little or none of permafrost carbon release from soils, streams, and wildfire: an expert assessment

Publication Type:

Journal Article

Source:

Environmental Research Letters, Volume 11, Number 3, p.13 (2016)

ISBN:

1748-9326

Accession Number:

WOS:000373401400017

Other Number:

146

URL:

http://apps.webofknowledge.com/InboundService.do?Func=Frame&amp;product=WOS&amp;action=retrieve&amp;mode=FullRecord&amp;UT=WOS:000373401400017

Keywords:

Arctic, ARCTIC TUNDRA, boreal, BOREAL FOREST, CLIMATE-CHANGE, coastal erosion, dissolved organic carbon, ECOSYSTEMS, Environmental Sciences, FIRE, INTERIOR ALASKA, Meteorology & Atmospheric Sciences, NITROGEN DEPOSITION, particulate organic carbon, permafrost carbon, SEQUESTRATION, STORAGE, VULNERABILITY, wildfire

Abstract:

As the permafrost region warms, its large organic carbon pool will be increasingly vulnerable to decomposition, combustion, and hydrologic export. Models predict that some portion of this release will be offset by increased production of Arctic and boreal biomass; however, the lack of robust estimates of net carbon balance increases the risk of further overshooting international emissions targets. Precise empirical or model-based assessments of the critical factors driving carbon balance are unlikely in the near future, so to address this gap, we present estimates from 98 permafrost-region experts of the response of biomass, wildfire, and hydrologic carbon flux to climate change. Results suggest that contrary to model projections, total permafrost-region biomass could decrease due to water stress and disturbance, factors that are not adequately incorporated in current models. Assessments indicate that end-of-the-century organic carbon release from Arctic rivers and collapsing coastlines could increase by 75% while carbon loss via burning could increase four-fold. Experts identified water balance, shifts in vegetation community, and permafrost degradation as the key sources of uncertainty in predicting future system response. In combination with previous findings, results suggest the permafrost region will become a carbon source to the atmosphere by 2100 regardless of warming scenario but that 65%-85% of permafrost carbon release can still be avoided if human emissions are actively reduced.

Notes:

ISI Document Delivery No.: DI3LY<br/>Times Cited: 5<br/>Cited Reference Count: 86<br/>Abbott, Benjamin W. Jones, Jeremy B. Schuur, Edward A. G. Chapin, F. Stuart, III Bowden, William B. Bret-Harte, M. Syndonia Epstein, Howard E. Flannigan, Michael D. Harms, Tamara K. Hollingsworth, Teresa N. Mack, Michelle C. McGuire, A. David Natali, Susan M. Rocha, Adrian V. Tank, Suzanne E. Turetsky, Merritt R. Vonk, Jorien E. Wickland, Kimberly P. Aiken, George R. Alexander, Heather D. Amon, Rainer M. W. Benscoter, Brian W. Bergeron, Yves Bishop, Kevin Blarquez, Olivier Bond-Lamberty, Ben Breen, Amy L. Buffam, Ishi Cai, Yihua Carcaillet, Christopher Carey, Sean K. Chen, Jing M. Chen, Han Y. H. Christensen, Torben R. Cooper, Lee W. Cornelissen, J. Hans C. de Groot, William J. DeLuca, Thomas H. Dorrepaal, Ellen Fetcher, Ned Finlay, Jacques C. Forbes, Bruce C. French, Nancy H. F. Gauthier, Sylvie Girardin, Martin P. Goetz, Scott J. Goldammer, Johann G. Gough, Laura Grogan, Paul Guo, Laodong Higuera, Philip E. Hinzman, Larry Hu, Feng Sheng Hugelius, Gustaf Jafarov, Elchin E. Jandt, Randi Johnstone, Jill F. Karlsson, Jan Kasischke, Eric S. Kattner, Gerhard Kelly, Ryan Keuper, Frida Kling, George W. Kortelainen, Pirkko Kouki, Jari Kuhry, Peter Laudon, Hjalmar Laurion, Isabelle Macdonald, Robie W. Mann, Paul J. Martikainen, Pertti J. McClelland, James W. Molau, Ulf Oberbauer, Steven F. Olefeldt, David Pare, David Parisien, Marc-Andre Payette, Serge Peng, Changhui Pokrovsky, Oleg S. Rastetter, Edward B. Raymond, Peter A. Raynolds, Martha K. Rein, Guillermo Reynolds, James F. Robards, Martin Rogers, Brendan M. Schaedel, Christina Schaefer, Kevin Schmidt, Inger K. Shvidenko, Anatoly Sky, Jasper Spencer, Robert G. M. Starr, Gregory Striegl, Robert G. Teisserenc, Roman Tranvik, Lars J. Virtanen, Tarmo Welker, Jeffrey M. Zimov, Sergei<br/>JAFAROV, ELCHIN/G-1616-2016; Macdonald, Robie/A-7896-2012; Tank, Suzanne/I-4816-2012; Carcaillet, Christopher/G-1218-2011; Cooper, Lee/E-5251-2012; Shvidenko, Anatoly/I-1505-2016; Finlay, Jacques/B-6081-2011; Benscoter, Brian/K-8105-2016; Bond-Lamberty, Ben/C-6058-2008; Raymond, Peter/C-4087-2009; Forbes, Bruce/L-4431-2013; Chen, Han/A-1359-2008; McClelland, James/C-5396-2008<br/>JAFAROV, ELCHIN/0000-0002-8310-3261; Rastetter, Edward/0000-0002-8620-5431; Macdonald, Robie/0000-0002-1141-8520; Tank, Suzanne/0000-0002-5371-6577; Carcaillet, Christopher/0000-0002-6632-1507; Cooper, Lee/0000-0001-7734-8388; Shvidenko, Anatoly/0000-0001-7640-2151; Finlay, Jacques/0000-0002-7968-7030; Benscoter, Brian/0000-0002-2706-4667; Bond-Lamberty, Ben/0000-0001-9525-4633; Raymond, Peter/0000-0002-8564-7860; Forbes, Bruce/0000-0002-4593-5083; Chen, Han/0000-0001-9477-5541; McClelland, James/0000-0001-9619-8194<br/>National Science Foundation ARCSS program and Vulnerability of Permafrost Carbon Research Coordination Network [OPP-0806465, OPP-0806394, 955713]; SITES (Swedish Science Foundation); Future Forest (Mistra); Marie Curie International Reintegration Grant within the 7th European Community Framework Programme. [277059]<br/>Peter J Fix provided valuable input on the methods and manuscript. This work was supported by the National Science Foundation ARCSS program and Vulnerability of Permafrost Carbon Research Coordination Network (grants OPP-0806465, OPP-0806394, and 955713) with additional funding from SITES (Swedish Science Foundation), Future Forest (Mistra), and a Marie Curie International Reintegration Grant (TOMCAR-Permafrost #277059) within the 7th European Community Framework Programme. This work complies with the US HHS Policy for Protection of Human Research Subjects. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the US Government.<br/>5<br/>48<br/>59<br/>IOP PUBLISHING LTD<br/>BRISTOL<br/>ENVIRON RES LETT