globalchange  > 气候减缓与适应
DOI: 10.1007/s10533-017-0414-x
Scopus记录号: 2-s2.0-85039751074
论文题名:
Wetland flux controls: how does interacting water table levels and temperature influence carbon dioxide and methane fluxes in northern Wisconsin?
作者: Pugh C.A.; Reed D.E.; Desai A.R.; Sulman B.N.
刊名: Biogeochemistry
ISSN: 0168-2563
EISSN: 1573-515X
出版年: 2018
卷: 137, 期:2018-01-02
起始页码: 15
结束页码: 25
语种: 英语
英文关键词: Carbon flux ; Eddy covariance ; Wetlands
英文摘要: Wetlands play a disproportionately large role in global terrestrial carbon stocks, and from 1 year to the next individual wetlands can fluctuate between carbon sinks and sources depending on factors such as hydrology, temperature, and land use. Although much research has been done on short-term seasonal to annual wetland biogeochemical cycles, there is a lack of experimental evidence concerning how the reversibility of wetland hydrological changes will influence these cycles over longer time periods. Five years of drought-induced declining water table at Lost Creek, a shrub fen wetland in northern Wisconsin, coincided with increased ecosystem respiration (Reco) and gross primary production (GPP) as derived from long-term eddy covariance observations. Since then, however, the average water table level at this site has increased, providing a unique opportunity to explore how wetland carbon fluxes are affected by interannual air temperature differences as well as changing water table levels. Water table level, as measured by water discharge, was correlated with Reco and GPP at interannual time scales. However, air temperature had a strong correlation with Reco, GPP, and net ecosystem productivity (NEP) at monthly time scales and correlated with NEP at inter-annual time scales. Methane flux was strongly temperature-controlled at seasonal time scales, increasing an order of magnitude from April to July. Annual methane emissions were 51 g C m−2. Our results demonstrate that over multi-year timescales, water table fluctuations can have limited effects on wetland net carbon fluxes and instead at Lost Creek annual temperature is the best predictor of interannual variation. © 2017, Springer International Publishing AG, part of Springer Nature.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/83189
Appears in Collections:气候减缓与适应
气候变化事实与影响

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作者单位: Department of Environmental Science, University of Virginia, Charlottesville, VA, United States; Department of Atmospheric and Oceanic Sciences, University of Wisconsin-Madison, Madison, WI, United States; Center for Global Change and Earth Observations, Michigan State University, East Lansing, MI, United States; Program in Atmospheric and Oceanic Sciences, Princeton University, Princeton, NJ, United States

Recommended Citation:
Pugh C.A.,Reed D.E.,Desai A.R.,et al. Wetland flux controls: how does interacting water table levels and temperature influence carbon dioxide and methane fluxes in northern Wisconsin?[J]. Biogeochemistry,2018-01-01,137(2018-01-02)
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