Effects of rising atmospheric CO2, climate change, and nitrogen deposition on aboveground net primary production in a temperate forest

被引:14
|
作者
Wang, Wen J. [2 ,3 ]
Ma, Shuang [1 ,2 ]
He, Hong S. [3 ]
Liu, Zhihua [4 ]
Thompson, Frank R., III [5 ]
Jin, Wenchi [3 ]
Wu, Zheng Fang [1 ]
Spetich, Martin A. [6 ]
Wang, Lei [2 ]
Xue, Song [2 ]
Zhang, Wenguang [2 ]
Wang, Xianwei [2 ]
机构
[1] Northeast Normal Univ, Sch Geog Sci, Minist Educ, Key Lab Geog Proc & Ecol Secur Changbai Mt, Changchun 130024, Jilin, Peoples R China
[2] Chinese Acad Sci, Northeast Inst Geog & Agroecol, Changchun 130102, Jilin, Peoples R China
[3] Univ Missouri, Sch Nat Resources, 203 ABNR Bldg, Columbia, MO 65211 USA
[4] Chinese Acad Sci, Inst Appl Ecol, CAS Key Lab Forest Ecol & Management, Shenyang 110016, Liaoning, Peoples R China
[5] US Forest Serv, USDA, Northern Res Stn, 202 ABNR Bldg, Columbia, MO 65211 USA
[6] US Forest Serv, Arkansas Forestry Sci Lab, USDA, Southern Res Stn, POB 1270, Hot Springs, AR 71902 USA
基金
中国国家自然科学基金;
关键词
carbon sink; forest productivity; ecosystem modeling; PnET; net primary production (NPP); temperate forest; TREE SPECIES DISTRIBUTION; LAND-USE HISTORY; CARBON SEQUESTRATION; NORTHERN WISCONSIN; PHOTOSYNTHESIS; DYNAMICS; IMPACTS; LEAF; LANDSCAPE; EXCHANGE;
D O I
10.1088/1748-9326/ab3178
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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 CO2 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 CO2 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 CO2 and N deposition enhanced ANPP (+0.253, +0.014 kg C m(-2) yr(-1)); (2) climate change interacted with rising CO2 and N deposition to decrease ANPP (-0.032, -0.018 kg C m(-2) yr(-1)); rising CO2 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 CO2 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.
引用
收藏
页数:10
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