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0344919328
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note
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In the model applied by Sarmiento and colleagues (7, 11), the most important changes occur in the Southern Ocean. A different mixing scheme results in a smaller change in the Southern Ocean (8).
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17
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0344919323
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19
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0344488157
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2 only differs by ∼ 10% from the forcing by all gases and aerosols, except for the two lowest stabilization profiles. The deviations are small in comparison to the overall range of forcings considered.
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22
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0344919287
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J. T. Houghton, L. G. Meira Filho, D. J. Griggs, K. Maskell, Eds. Intergovernmental Panel on Climate Change, Geneva
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D. Schimel et al., in IPCC Technical Paper III, Stabilisation of Atmospheric Greenhouse Gases: Physical, Biological, and Socio-economic Implications, J. T. Houghton, L. G. Meira Filho, D. J. Griggs, K. Maskell, Eds. (Intergovernmental Panel on Climate Change, Geneva, 1997), pp. 1-48.
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Schimel, D.1
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25
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0344488138
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The attribution of the carbon uptake reduction to different mechanisms is only an approximation because the ocean-atmosphere carbon cycle system is nonlinear. The validity of our attribution was checked by running additional simulations and an inorganic model.
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26
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0344919294
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2 air-sea fluxes.
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0345350517
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2.
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31
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0344488135
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note
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We thank E. Maier-Reimer for helpful comments. This work was supported by the European Commission Programme Climate and Environment (grants ENV4-CT97-0495, ENV4-CT95-0130, ENV4-CT95-0131, and ENV4-CT97-0643), the Swiss Federal Office for Science and Education (grants 97.0414, 95.0470, 95.0471, and 97.0414), and the Swiss National Science Foundation.
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