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The contribution of China’s emissions to global climate forcing

Author

Listed:
  • Bengang Li

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University
    Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application)

  • Thomas Gasser

    (Laboratoire des Sciences du Climat et de l’Environnement, CEA-CNRS-UVSQ
    Centre International de Recherche en Environnement et Développement, CNRS-PontsParisTech-EHESS-AgroParisTech-CIRAD)

  • Philippe Ciais

    (Laboratoire des Sciences du Climat et de l’Environnement, CEA-CNRS-UVSQ)

  • Shilong Piao

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University
    Key Laboratory of Alpine Ecology and Biodiversity, Institute of Tibetan Plateau Research, Center for Excellence in Tibetan Earth Science, Chinese Academy of Sciences)

  • Shu Tao

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

  • Yves Balkanski

    (Laboratoire des Sciences du Climat et de l’Environnement, CEA-CNRS-UVSQ)

  • Didier Hauglustaine

    (Laboratoire des Sciences du Climat et de l’Environnement, CEA-CNRS-UVSQ)

  • Juan-Pablo Boisier

    (Laboratoire des Sciences du Climat et de l’Environnement, CEA-CNRS-UVSQ)

  • Zhuo Chen

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

  • Mengtian Huang

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

  • Laurent Zhaoxin Li

    (Laboratoire de Météorologie Dynamique, CNRS, Université Pierre et)

  • Yue Li

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

  • Hongyan Liu

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

  • Junfeng Liu

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

  • Shushi Peng

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

  • Zehao Shen

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

  • Zhenzhong Sun

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

  • Rong Wang

    (Laboratoire des Sciences du Climat et de l’Environnement, CEA-CNRS-UVSQ)

  • Tao Wang

    (Laboratoire des Sciences du Climat et de l’Environnement, CEA-CNRS-UVSQ)

  • Guodong Yin

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

  • Yi Yin

    (Laboratoire des Sciences du Climat et de l’Environnement, CEA-CNRS-UVSQ)

  • Hui Zeng

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

  • Zhenzhong Zeng

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

  • Feng Zhou

    (Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University)

Abstract

Using a global coupled biogeochemistry–climate model and a chemistry and transport model reveals that China’s present-day global radiative forcing is about ten per cent of the current global total, made up of both warming and cooling contributions; if in the future China reduces the cooling forcings, global warming could accelerate.

Suggested Citation

  • Bengang Li & Thomas Gasser & Philippe Ciais & Shilong Piao & Shu Tao & Yves Balkanski & Didier Hauglustaine & Juan-Pablo Boisier & Zhuo Chen & Mengtian Huang & Laurent Zhaoxin Li & Yue Li & Hongyan Li, 2016. "The contribution of China’s emissions to global climate forcing," Nature, Nature, vol. 531(7594), pages 357-361, March.
  • Handle: RePEc:nat:nature:v:531:y:2016:i:7594:d:10.1038_nature17165
    DOI: 10.1038/nature17165
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    Cited by:

    1. Lee, Chien-Chiang & Wang, Fuhao & Lou, Runchi & Wang, Keying, 2023. "How does green finance drive the decarbonization of the economy? Empirical evidence from China," Renewable Energy, Elsevier, vol. 204(C), pages 671-684.
    2. Qingyang Wu & Siyu Ren & Yao Hou & Zaoli Yang & Congyu Zhao & Xusheng Yao, 2024. "Easing financial constraints through carbon trading," Empirical Economics, Springer, vol. 67(2), pages 655-691, August.

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