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Effects of rising atmospheric CO 2 , climate change, and nitrogen deposition on aboveground net primary production in a temperate forest

Bibliographic Data

ID15550684
AuthorsWen J Wang (0000-0002-2769-671X, University of Missouri, corresponding author), Shuang Ma (0000-0001-7125-5279, Chinese Academy of Sciences), Hong S He (0000-0002-3983-2512, University of Missouri, corresponding author), Zhihua Liu (0000-0001-5784-9724, Institute of Applied Ecology), Frank R Thompson (0000-0002-5848-906X, Northern Research Station), Wenchi Jin (University of Missouri), Zheng Fang Wu (Northeast Normal University, corresponding author), Martín A Spetich (Southern Research Station), Lei Wang (0000-0001-5326-565X, Chinese Academy of Sciences, corresponding author), Song Xue (0000-0001-5058-9229, Chinese Academy of Sciences), Wenguang Zhang (0000-0003-0160-0342, Northeast Institute of Geography and Agroecology), Xianwei Wang (0009-0007-4801-1736, Chinese Academy of Sciences, corresponding author)
Year2019
Volume14
Issue10
Pages104005-104005
Publication date2019-07-11
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ab3178
OpenAlexW2960311433
LanguageEN
References cited54

Temperate forests regrowing from historical land use and land cover change in the eastern US serve as carbon (C) sinks. Environmental drivers have been significantly altered (e.g. rising atmospheric CO 2 concentration, warmer temperature, and elevated nitrogen (N) deposition) and will have a wide range of impacts on future forest C sinks. However, the interactions among these environmental drivers are unclear and their effects are subject to uncertainty. We assessed the combined and interactive effects of rising CO 2 concentration, climate change (temperature, precipitation), and N deposition on forest aboveground net primary production (ANPP) and their relative contribution to ANPP changes of a temperate forest in the eastern US. We used a process-based ecosystem model PnET-day to simulate coupled cycles of C, water, and N of forest ecosystems. We found that (1) climate change exerted negative effects on ANPP (−0.250 kg C m −2 yr −1 ) whereas rising CO 2 and N deposition enhanced ANPP (+0.253, +0.014 kg C m −2 yr −1 ); (2) climate change interacted with rising CO 2 and N deposition to decrease ANPP (−0.032, −0.018 kg C m −2 yr −1 ); rising CO 2 and N deposition acted in synergy to increase ANPP (+0.014 kg C m −2 yr −1 ); (3) changes in ANPP were mainly attributed to rising CO 2 and climate change whereas N deposition effects and any two- or three-factor interactive effects were relatively small. Our results suggest that the total negative effect sizes will not be offset by the total positive effect sizes, thus resulting in reductions in forest ANPP over the 21st century

Atmospheric sciences · Biology · Carbon sink · Climate change · Deposition (geology · Ecosystem · Geography · Meteorology · Nitrogen · Precipitation · Primary production · Temperate climate · Temperate forest · Temperate rainforest · Atmospheric and Environmental Gas Dynamics · Chemistry · Environmental Science · Plant responses to elevated CO2 · Plant Water Relations and Carbon Dynamics · Ecology · Geology

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