Factors controlling large scale variations in methane emissions from wetlands -: art. no. 1414

被引:259
作者
Christensen, TR [1 ]
Ekberg, A
Ström, L
Mastepanov, M
Panikov, N
Öquist, M
Svensson, BH
Nykänen, H
Martikainen, PJ
Oskarsson, H
机构
[1] Lund Univ, GeoBiosphere Sci Ctr, Dept Phys Geog & Ecosyst Anal, S-22362 Lund, Sweden
[2] Stevens Inst Technol, Dept Chem & Biol Chem, Hoboken, NJ 07030 USA
[3] Linkoping Univ, Dept Water & Environm Studies, S-58183 Linkoping, Sweden
[4] Univ Kuopio, Dept Environm Sci, FIN-70211 Kuopio, Finland
[5] RALA, Agr Res Inst, IS-112 Reykjavik, Iceland
关键词
D O I
10.1029/2002GL016848
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
[1] Global wetlands are, at estimate ranging 115-237 Tg CH4/yr, the largest single atmospheric source of the greenhouse gas methane (CH4). We present a dataset on CH4 flux rates totaling 12 measurement years at sites from Greenland, Iceland, Scandinavia and Siberia. We find that temperature and microbial substrate availability (expressed as the organic acid concentration in peat water) combined explain almost 100% of the variations in mean annual CH4 emissions. The temperature sensitivity of the CH4 emissions shown suggests a feedback mechanism on climate change that could validate incorporation in further developments of global circulation models.
引用
收藏
页码:67 / 1
页数:4
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