气候变化领域集成服务门户(CCPortal): Permafrost carbon-climate feedbacks accelerate global warming

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DOI	10.1073/pnas.1103910108
	Permafrost carbon-climate feedbacks accelerate global warming
	Koven C.D.; Ringeval B.; Friedlingstein P.; Ciais P.; Cadule P.; Khvorostyanov D.; Krinner G.; Tarnocai C.
发表日期	2011
ISSN	0027-8424
起始页码	14769
结束页码	14774
卷号	108 期号:36
英文摘要	Permafrost soils contain enormous amounts of organic carbon, which could act as a positive feedback to global climate change due to enhanced respiration rates with warming. We have used a terrestrial ecosystem model that includes permafrost carbon dynamics, inhibition of respiration in frozen soil layers, vertical mixing of soil carbon from surface to permafrost layers, and CH 4 emissions from flooded areas, and which better matches new circumpolar inventories of soil carbon stocks, to explore the potential for carbon-climate feedbacks at high latitudes. Contrary to model results for the Intergovernmental Panel on Climate Change Fourth Assessment Report (IPCC AR4), when permafrost processes are included, terrestrial ecosystems north of 60° N could shift from being a sink to a source of CO 2 by the end of the 21st century when forced by a Special Report on Emissions Scenarios (SRES) A2 climate change scenario. Between 1860 and 2100, the model response to combined CO 2 fertilization and climate change changes from a sink of 68 Pg to a 27 + -7 Pg sink to 4 + -18 Pg source, depending on the processes and parameter values used. The integrated change in carbon due to climate change shifts from near zero, which is within the range of previous model estimates, to a climate-induced loss of carbon by ecosystems in the range of 25 + -3 to 85+ -16 Pg C, depending on processes included in the model, with a best estimate of a 62 + -7 Pg C loss. Methane emissions from high-latitude regions are calculated to increase from 34 Tg CH 4/y to 41-70 TgCH 4/y, with increases due to CO 2 fertilization, permafrost thaw, and warming-induced increased CH 4 flux densities partially offset by a reduction in wetland extent.
英文关键词	Active layer; Carbon cycle; Cryosphere; Land surface models; Soil organic matter
语种	英语
scopus关键词	methane; organic carbon; article; carbon footprint; climate; climate change; ecosystem; environmental temperature; greenhouse effect; latitude; permafrost; priority journal; soil; wetland; Carbon; Cold Climate; Global Warming; Models, Theoretical
来源期刊	Proceedings of the National Academy of Sciences of the United States of America
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/158940
作者单位	Koven, C.D., Laboratoire des Sciences du Climat et de l'Environnement, Centre National de la Recherche Scientifique, Commissariat à l'Energie Atomique, 91191 Gif-sur-Yvette, France, Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, United States; Ringeval, B., Laboratoire des Sciences du Climat et de l'Environnement, Centre National de la Recherche Scientifique, Commissariat à l'Energie Atomique, 91191 Gif-sur-Yvette, France; Friedlingstein, P., College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter EX4 4QF, United Kingdom; Ciais, P., Laboratoire des Sciences du Climat et de l'Environnement, Centre National de la Recherche Scientifique, Commissariat à l'Energie Atomique, 91191 Gif-sur-Yvette, France; Cadule, P., Laboratoire des Sciences du Climat et de l'Environnement, Centre National de la Recherche Scientifique, Commissariat à l'Energie Atomique, 91191 Gif-sur-Yvette, France; Khvorostyanov, D., Laboratoire de Météorologie Dynamique, Ecol...
推荐引用方式 GB/T 7714	Koven C.D.,Ringeval B.,Friedlingstein P.,et al. Permafrost carbon-climate feedbacks accelerate global warming[J],2011,108(36).
APA	Koven C.D..,Ringeval B..,Friedlingstein P..,Ciais P..,Cadule P..,...&Tarnocai C..(2011).Permafrost carbon-climate feedbacks accelerate global warming.Proceedings of the National Academy of Sciences of the United States of America,108(36).
MLA	Koven C.D.,et al."Permafrost carbon-climate feedbacks accelerate global warming".Proceedings of the National Academy of Sciences of the United States of America 108.36(2011).