Top–down assessment of the Asian carbon budget since the mid 1990s

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作者
R. L. Thompson
P. K. Patra
F. Chevallier
S. Maksyutov
R. M. Law
T. Ziehn
I. T. van der Laan-Luijkx
W. Peters
A. Ganshin
R. Zhuravlev
T. Maki
T. Nakamura
T. Shirai
M. Ishizawa
T. Saeki
T. Machida
B. Poulter
J. G. Canadell
P. Ciais
机构
[1] Norsk Institutt for Luftforskning (NILU),Department of Environmental Geochemical Cycle Research
[2] Japan Agency for Marine Earth Science and Technology (JAMSTEC),Department of Meteorology and Air Quality
[3] Laboratoire des Sciences du Climat et l’Environnement (LSCE,Department of Upper Atmospheric Layers Physics
[4] CEA-CNRS-UVSQ),Department of Atmospheric Physics and Microwave Diagnostics
[5] National Institute for Environmental Studies (NIES),Atmospheric Environment and Applied Meteorology Research Department
[6] Oceans and Atmosphere,Global Environment and Marine Department
[7] Commonwealth Scientific and Industrial Research Organisation (CSIRO),Institute on Ecosystems and Department of Ecology
[8] Environmental Sciences Group,undefined
[9] Wageningen University (WU),undefined
[10] University of Groningen,undefined
[11] Centre for Isotope Research,undefined
[12] Central Aerological Observatory (CAO),undefined
[13] National Research Tomsk State University (TSU),undefined
[14] Institute of Applied Physics of the Russian Academy of Sciences,undefined
[15] Meteorological Research Institute (MRI),undefined
[16] Japan Meteorological Agency (JMA),undefined
[17] Montana State University (MSU),undefined
[18] Global Carbon Project,undefined
[19] Commonwealth Scientific and Industrial Research Organisation (CSIRO),undefined
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摘要
Increasing atmospheric carbon dioxide (CO2) is the principal driver of anthropogenic climate change. Asia is an important region for the global carbon budget, with 4 of the world’s 10 largest national emitters of CO2. Using an ensemble of seven atmospheric inverse systems, we estimated land biosphere fluxes (natural, land-use change and fires) based on atmospheric observations of CO2 concentration. The Asian land biosphere was a net sink of −0.46 (−0.70–0.24) PgC per year (median and range) for 1996–2012 and was mostly located in East Asia, while in South and Southeast Asia the land biosphere was close to carbon neutral. In East Asia, the annual CO2 sink increased between 1996–2001 and 2008–2012 by 0.56 (0.30–0.81) PgC, accounting for ∼35% of the increase in the global land biosphere sink. Uncertainty in the fossil fuel emissions contributes significantly (32%) to the uncertainty in land biosphere sink change.
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