An atmospheric perspective on North American carbon dioxide exchange:: CarbonTracker

被引:788
作者
Peters, Wouter
Jacobson, Andrew R.
Sweeney, Colm
Andrews, Arlyn E.
Conway, Thomas J.
Masarie, Kenneth
Miller, John B.
Bruhwiler, Lori M. P.
Petron, Gabrielle
Hirsch, Adam I.
Worthy, Douglas E. J.
van der Werf, Guido R.
Randerson, James T.
Wennberg, Paul O.
Krol, Maarten C.
Tans, Pieter P.
机构
[1] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA
[2] Cooperat Inst Res Environm Sci, UCB 216, Boulder, CO 80303 USA
[3] Environm Canada, Toronto, ON M3H 5T4, Canada
[4] Vrije Univ Amsterdam, Fac Earth & Life Sci, NL-1081 HV Amsterdam, Netherlands
[5] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA
[6] CALTECH, Div Engn & Appl Sci, Pasadena, CA 91125 USA
[7] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
[8] Univ Wageningen & Res Ctr, Dept Meteorol & Air Qual, NL-6708 PB Wageningen, Netherlands
关键词
carbon cycle; greenhouse gases; data assimilation; biogeochemistry; atmospheric composition;
D O I
10.1073/pnas.0708986104
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
We present an estimate of net CO2 exchange between the terrestrial biosphere and the atmosphere across North America for every week in the period 2000 through 2005. This estimate is derived from a set of 28,000 CO2 mole fraction observations in the global atmosphere that are fed into a state-of-the-art data assimilation system for CO2 called CarbonTracker. By design, the surface fluxes produced in CarbonTracker are consistent with the recent history Of CO2 in the atmosphere and provide constraints on the net carbon flux independent from national inventories derived from accounting efforts. We find the North American terrestrial biosphere to have absorbed -0.65 PgC/yr (1 petagram = 10(15) g; negative signs are used for carbon sinks) averaged over the period studied, partly offsetting the estimated 1.85 PgC/yr release by fossil fuel burning and cement manufacturing. Uncertainty on this estimate is derived from a set of sensitivity experiments and places the sink within a range of -0.4 to -1.0 PgC/yr. The estimated sink is located mainly in the deciduous forests along the East Coast (32%) and the boreal coniferous forests (22%). Terrestrial uptake fell to -0.32 PgC/yr during the large-scale drought of 2002, suggesting sensitivity of the contemporary carbon sinks to climate extremes. CarbonTracker results are in excellent agreement with a wide collection of carbon inventories that form the basis of the first North American State of the Carbon Cycle Report (SOCCR), to be released in 2007. All CarbonTracker results are freely available at http://carbontracker.noaa.gov.
引用
收藏
页码:18925 / 18930
页数:6
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