Increased atmospheric vapor pressure deficit reduces global vegetation growth
Author(s) -
Wenping Yuan,
Yi Zheng,
Shilong Piao,
Philippe Ciais,
Danica Lombardozzi,
YingPing Wang,
Youngryel Ryu,
Guixing Chen,
Wenjie Dong,
HU Zhong-ming,
Atul K. Jain,
Chongya Jiang,
Etsushi Kato,
Shihua Li,
Sebastian Lienert,
Shuguang Liu,
Julia E. M. S. Nabel,
Zhangcai Qin,
Timothy A. Quine,
Stephen Sitch,
William K. Smith,
F. Wang,
Chaoyang Wu,
Zhiqiang Xiao,
Song Yang
Publication year - 2019
Publication title -
science advances
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 5.928
H-Index - 146
ISSN - 2375-2548
DOI - 10.1126/sciadv.aax1396
Subject(s) - greening , vegetation (pathology) , environmental science , vapour pressure deficit , atmospheric pressure , atmospheric sciences , water vapor , climatology , meteorology , ecology , geography , transpiration , photosynthesis , biology , medicine , geology , botany , pathology
Atmospheric vapor pressure deficit (VPD) is a critical variable in determining plant photosynthesis. Synthesis of four global climate datasets reveals a sharp increase of VPD after the late 1990s. In response, the vegetation greening trend indicated by a satellite-derived vegetation index (GIMMS3g), which was evident before the late 1990s, was subsequently stalled or reversed. Terrestrial gross primary production derived from two satellite-based models (revised EC-LUE and MODIS) exhibits persistent and widespread decreases after the late 1990s due to increased VPD, which offset the positive CO fertilization effect. Six Earth system models have consistently projected continuous increases of VPD throughout the current century. Our results highlight that the impacts of VPD on vegetation growth should be adequately considered to assess ecosystem responses to future climate conditions.
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