Isolating and Quantifying the Effects of Climate and CO2 Changes (1980-2014) on the Net Primary Productivity in Arid and Semiarid China

被引:58
|
作者
Fang, Xia [1 ,2 ,3 ,4 ]
Zhang, Chi [1 ]
Wang, Quan [5 ]
Chen, Xi [1 ]
Ding, Jianli [2 ]
Karamage, Fidele [1 ,3 ]
机构
[1] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, Urumqi 830011, Xinjiang, Peoples R China
[2] Xinjiang Univ, Sch Resources & Environm, Xinjiang 830046, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[4] Xinjiang Polytech Coll, Urumqi 830091, Xinjiang, Peoples R China
[5] Shizuoka Univ, Fac Agr, Shizuoka 4228529, Japan
来源
FORESTS | 2017年 / 8卷 / 03期
基金
美国国家科学基金会;
关键词
AEM model; net primary productivity (NPP); climate change; CO2 fertilization effect; arid; semiarid China; ELEVATED ATMOSPHERIC CO2; LAND-USE CHANGE; CARBON DYNAMICS; DESERT SHRUBS; GROWTH; ENRICHMENT; MODEL; RESPONSES; SURFACE; SOIL;
D O I
10.3390/f8030060
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Although the net primary productivity (NPP) of arid/semiarid ecosystem is generally thought to be controlled by precipitation, other factors like CO2 fertilization effect and temperature change may also have important impacts, especially in the cold temperate areas of the northern China, where significant warming was reported in the recent decades. However, the impacts of climate and atmospheric CO2 changes to the NPP dynamics in the arid and semiarid areas of China (ASA-China) is still unclear, hindering the development of climate adaptation strategy. Based on numeric experiments and factorial analysis, this study isolated and quantified the effects of climate and CO2 changes between 1980-2014 on ASA-China's NPP, using the Arid Ecosystem Model (AEM) that performed well in predicting ecosystems' responses to climate/CO2 change according to our evaluation based on 21 field experiments. Our results showed that the annual variation in NPP was dominated by changes in precipitation, which reduced the regional NPP by 10.9 g.C/(m(2).year). The precipitation-induced loss, however, has been compensated by the CO2 fertilization effect that increased the regional NPP by 14.9 g.C/(m(2).year). The CO2 fertilization effect particularly benefited the extensive croplands in the Northern China Plain, but was weakened in the dry grassland of the central Tibetan Plateau due to suppressed plant activity as induced by a drier climate. Our study showed that the climate change in ASA-China and the ecosystem's responses were highly heterogeneous in space and time. There were complex interactive effects among the climate factors, and different plant functional types (e.g., phreatophyte vs. non-phreatophyte) could have distinct responses to similar climate change. Therefore, effective climate-adaptive strategies should be based on careful analysis of local climate pattern and understanding of the characteristic responses of the dominant species. Particularly, China's policy makers should pay close attention to climate change and ecosystem health in northeastern China, where significant loss in forest NPP has been triggered by drought, and carefully balance the ecological and agricultural water usage. For wildlife conservation, the drought-stressed grassland in the central Tibetan Plateau should be protected from overgrazing in the face of dramatic warming in the 21st century.
引用
收藏
页数:19
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