What determines the magnitude of carbon cycle-climate feedbacks?

被引:46
|
作者
Matthews, H. Damon
Eby, Michael
Ewen, Tracy
Friedlingstein, Pierre
Hawkins, Barbara J.
机构
[1] Concordia Univ, Dept Geog Planning & Environm, Montreal, PQ H3G 1M8, Canada
[2] Univ Victoria, Sch Earth & Ocean Sci, Stn CSC, Victoria, BC V8W 3P6, Canada
[3] ETH, Inst Atmospher & Climate Sci, CH-8092 Zurich, Switzerland
[4] Inst Pierre Simon Laplace, LSCE, F-91191 Gif Sur Yvette, France
[5] Univ Victoria, Ctr Forest Biol, Victoria, BC V8W 3P6, Canada
关键词
D O I
10.1029/2006GB002733
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
[1] Positive feedbacks between climate change and the carbon cycle have the potential to amplify the growth of atmospheric carbon dioxide and accelerate future climate warming. However, both the magnitude of and the processes which drive future carbon cycle-climate feedbacks remain highly uncertain. In this study, we use a coupled climate-carbon model to investigate how the response of vegetation photosynthesis to climate change contributes to the overall strength of carbon cycle-climate feedbacks. We find that the feedback strength is particularly sensitive to the model representation of the photosynthesis-temperature response, with lesser sensitivity to the parameterization of soil moisture and nitrogen availability. In all simulations, large feedbacks are associated with a climatic suppression of terrestrial primary productivity and consequent reduction of terrestrial carbon uptake. This process is particularly evident in the tropics and can explain a large part of the range of carbon cycle-climate feedbacks simulated by different coupled climate-carbon models.
引用
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页数:12
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