Sensitivity of the carbon cycle in the Arctic to climate change

被引:739
作者
McGuire, A. David [1 ]
Anderson, Leif G. [2 ]
Christensen, Torben R. [3 ]
Dallimore, Scott [4 ]
Guo, Laodong [5 ]
Hayes, Daniel J. [6 ]
Heimann, Martin [7 ]
Lorenson, Thomas D. [8 ]
Macdonald, Robie W. [9 ]
Roulet, Nigel [10 ,11 ]
机构
[1] Univ Alaska, Alaska Cooperat Fish & Wildlife Res Unit, US Geol Survey, Fairbanks, AK 99775 USA
[2] Univ Gothenburg, Dept Chem, SE-41296 Gothenburg, Sweden
[3] Lund Univ, Geobiosphere Sci Ctr, Lund, Sweden
[4] Geol Survey Canada, Sidney, BC V8L 4B2, Canada
[5] Univ So Mississippi, Dept Marine Sci, Stennis Space Ctr, MS 39529 USA
[6] Univ Alaska, Inst Arctic Biol, Fairbanks, AK 99775 USA
[7] Max Planck Inst Biogeochem, Jena, Germany
[8] US Geol Survey, Menlo Pk, CA 94025 USA
[9] Inst Ocean Sci, Dept Fisheries & Oceans, Sidney, BC V8L 4B2, Canada
[10] McGill Univ, Dept Geog, Montreal, PQ H3A 2K6, Canada
[11] McGill Univ, Sch Environm, Montreal, PQ H3A 2K6, Canada
基金
美国国家科学基金会; 美国海洋和大气管理局;
关键词
Arctic; Arctic Ocean; boreal forest; carbon cycle; carbon dioxide; climate change; climate feedbacks; hydrates; methane; permafrost; review; tundra; DISSOLVED ORGANIC-MATTER; TRACE GAS-EXCHANGE; MODERN METHANE EMISSIONS; NATURAL WETLANDS; ATMOSPHERIC METHANE; TERRESTRIAL ECOSYSTEMS; RUSSIAN FORESTS; NORTHERN ALASKA; CO2; EXCHANGE; DIOXIDE SUPERSATURATION;
D O I
10.1890/08-2025.1
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The recent warming in the Arctic is affecting a broad spectrum of physical, ecological, and human/cultural systems that may be irreversible on century time scales and have the potential to cause rapid changes in the earth system. The response of the carbon cycle of the Arctic to changes in climate is a major issue of global concern, yet there has not been a comprehensive review of the status of the contemporary carbon cycle of the Arctic and its response to climate change. This review is designed to clarify key uncertainties and vulnerabilities in the response of the carbon cycle of the Arctic to ongoing climatic change. While it is clear that there are substantial stocks of carbon in the Arctic, there are also significant uncertainties associated with the magnitude of organic matter stocks contained in permafrost and the storage of methane hydrates beneath both subterranean and submerged permafrost of the Arctic. In the context of the global carbon cycle, this review demonstrates that the Arctic plays an important role in the global dynamics of both CO2 and CH4. Studies suggest that the Arctic has been a sink for atmospheric CO2 of between 0 and 0.8 Pg C/yr in recent decades, which is between 0% and 25% of the global net land/ocean flux during the 1990s. The Arctic is a substantial source of CH4 to the atmosphere (between 32 and 112 Tg CH4/yr), primarily because of the large area of wetlands throughout the region. Analyses to date indicate that the sensitivity of the carbon cycle of the Arctic during the remainder of the 21st century is highly uncertain. To improve the capability to assess the sensitivity of the carbon cycle of the Arctic to projected climate change, we recommend that (1) integrated regional studies be conducted to link observations of carbon dynamics to the processes that are likely to influence those dynamics, and (2) the understanding gained from these integrated studies be incorporated into both uncoupled and fully coupled carbon-climate modeling efforts.
引用
收藏
页码:523 / 555
页数:33
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