Climate mitigation from vegetation biophysical feedbacks during the past three decades

Zhenzhong Zeng, Shilong Piao (), Laurent Z. X. Li, Liming Zhou, Philippe Ciais, Tao Wang, Yue Li, Xu Lian, Eric F. Wood, Pierre Friedlingstein, Jiafu Mao, Lyndon D. Estes, Ranga B. Myneni, Shushi Peng, Xiaoying Shi, Sonia I. Seneviratne and Yingping Wang
Additional contact information
Zhenzhong Zeng: Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University
Shilong Piao: Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University
Laurent Z. X. Li: Laboratoire de Météorologie Dynamique, Centre National de la Recherche Scientifique, Sorbonne Universités, UPMC Univ Paris 06
Liming Zhou: University at Albany, State University of New York
Philippe Ciais: Laboratoire des Sciences du Climat et de l’Environnement, UMR 1572 CEA-CNRS-UVSQ
Tao Wang: Key Laboratory of Alpine Ecology and Biodiversity, Institute of Tibetan Plateau Research, Chinese Academy of Sciences
Yue Li: Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University
Xu Lian: Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University
Eric F. Wood: Princeton University
Pierre Friedlingstein: College of Engineering, Mathematics and Physical Sciences, University of Exeter
Jiafu Mao: Oak Ridge National Laboratory
Lyndon D. Estes: Princeton University
Ranga B. Myneni: Boston University, Boston
Shushi Peng: Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University
Xiaoying Shi: Oak Ridge National Laboratory
Sonia I. Seneviratne: Institute for Atmospheric and Climate Science, ETH Zurich
Yingping Wang: CSIRO Oceans and Atmosphere

Nature Climate Change, 2017, vol. 7, issue 6, 432-436

Abstract: Greening—increasing leaf area index—affects regional climate in a number of contradictory ways. The net global effect is now revealed to be cooling that has offset the equivalent of 12% of global land-surface warming over the past 30 years.

Date: 2017
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DOI: 10.1038/nclimate3299

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