Large historical growth in global terrestrial gross primary production

被引:0
|
作者
J. E. Campbell
J. A. Berry
U. Seibt
S. J. Smith
S. A. Montzka
T. Launois
S. Belviso
L. Bopp
M. Laine
机构
[1] Sierra Nevada Research Institute,Department of Global Ecology
[2] University of California,Department of Atmospheric and Oceanic Sciences
[3] Carnegie Institution for Science,undefined
[4] University of California,undefined
[5] Los Angeles,undefined
[6] California 90095,undefined
[7] USA,undefined
[8] Joint Global Change Research Institute,undefined
[9] Pacific Northwest National Laboratory,undefined
[10] Earth System Research Laboratory,undefined
[11] National Oceanic and Atmospheric Administration,undefined
[12] Laboratoire des Sciences du Climat et de l’Environnement,undefined
[13] IPSL,undefined
[14] CNRS/CEA/UVSQ,undefined
[15] 91191 Gif sur Yvette,undefined
[16] France.,undefined
[17] Finnish Meteorological Institute,undefined
[18] †Present address: INRA,undefined
[19] UMR 1391 ISPA,undefined
[20] 33140 Villenave d’Ornon,undefined
[21] France (T.L.); Laboratoire de Météorologie Dynamique,undefined
[22] IPSL,undefined
[23] CNRS/ENS/UMPC/X,undefined
[24] 75005 Paris,undefined
[25] France (L.B.).,undefined
来源
Nature | 2017年 / 544卷
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学科分类号
摘要
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.
引用
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页码:84 / 87
页数:3
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