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Volumn 284, Issue 5413, 1999, Pages 464-467

Global warming and marine carbon cycle feedbacks on future atmospheric CO2

Author keywords

[No Author keywords available]

Indexed keywords

CARBON DIOXIDE;

EID: 0033574782     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.284.5413.464     Document Type: Article
Times cited : (255)

References (31)
  • 4
    • 0344056974 scopus 로고    scopus 로고
    • Max-Planck-Institut für Meteorologie, Hamburg, Germany
    • U. Mikolajewicz and R. Voss, Technical Report 263 (Max-Planck-Institut für Meteorologie, Hamburg, Germany, 1998), pp. 1-27.
    • (1998) Technical Report , vol.263 , pp. 1-27
    • Mikolajewicz, U.1    Voss, R.2
  • 9
    • 0032485386 scopus 로고    scopus 로고
    • B. Stauffer et al. Nature 392, 59 (1998).
    • (1998) Nature , vol.392 , pp. 59
    • Stauffer, B.1
  • 12
    • 0344919328 scopus 로고    scopus 로고
    • note
    • 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).
  • 17
    • 0344919323 scopus 로고    scopus 로고
    • note
    • 2 (21).
  • 19
    • 0344488157 scopus 로고    scopus 로고
    • note
    • 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.
  • 25
    • 0344488138 scopus 로고    scopus 로고
    • note
    • 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.
  • 26
    • 0344919294 scopus 로고    scopus 로고
    • note
    • 2 air-sea fluxes.
  • 27
    • 0345350517 scopus 로고    scopus 로고
    • note
    • 2.
  • 31
    • 0344488135 scopus 로고    scopus 로고
    • note
    • 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.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.