Large historical growth in global terrestrial gross primary production

J. E. Campbell (), J. A. Berry, U. Seibt, S. J. Smith, S. A. Montzka, T. Launois, S. Belviso, L. Bopp and M. Laine
Additional contact information
J. E. Campbell: Sierra Nevada Research Institute, University of California
J. A. Berry: Carnegie Institution for Science
U. Seibt: University of California, Los Angeles, California 90095, USA
S. J. Smith: Joint Global Change Research Institute, Pacific Northwest National Laboratory
S. A. Montzka: Earth System Research Laboratory, National Oceanic and Atmospheric Administration
T. Launois: Laboratoire des Sciences du Climat et de l’Environnement, IPSL, CNRS/CEA/UVSQ, 91191 Gif sur Yvette, France.
S. Belviso: Laboratoire des Sciences du Climat et de l’Environnement, IPSL, CNRS/CEA/UVSQ, 91191 Gif sur Yvette, France.
L. Bopp: Laboratoire des Sciences du Climat et de l’Environnement, IPSL, CNRS/CEA/UVSQ, 91191 Gif sur Yvette, France.
M. Laine: Finnish Meteorological Institute

Nature, 2017, vol. 544, issue 7648, 84-87

Abstract: Long-term records of global carbonyl sulfide levels reveal that terrestrial gross primary production (GPP) increased by around 30% during the twentieth century—a finding that may aid understanding of the connection between GPP growth and climate change.

Date: 2017
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DOI: 10.1038/nature22030

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