Arid
DOI10.1016/j.agrformet.2016.07.007
Carbon and water exchange over a temperate semi-arid shrubland during three years of contrasting precipitation and soil moisture patterns
Jia, Xin1,2,3; Zha, Tianshan1,2; Gong, Jinnan3; Wang, Ben1,2,3; Zhang, Yuqing1,2; Wu, Bin1,2; Qin, Shugao1,2; Peltola, Hell3
通讯作者Zha, Tianshan
来源期刊AGRICULTURAL AND FOREST METEOROLOGY
ISSN0168-1923
EISSN1873-2240
出版年2016
卷号228页码:120-129
英文摘要

Water is considered a key factor affecting ecosystem carbon exchange in dryland regions. However, the relationship between inter-annual variations in precipitation and ecosystem productivity remains to be clarified for arid and semi-arid areas. Based on eddy-covariance measurements, we examined how ecosystem production in a shrubland of northern China varied over three years (2012-2014) with contrasting precipitation and soil moisture patterns. Net ecosystem production (NEP) was 77 +/- 10 (+/- standard deviation), -4 +/- 10 and -22 +/- 5 g C m(-2) in 2012-2014, respectively, indicating a rapid shift from an annual sink to a source of carbon. Gross ecosystem production (GEP), total ecosystem respiration (TER) and evapotranspiration (ET) also declined over the three years. Annual carbon and water fluxes appeared to be suppressed in years with low spring soil moisture, which declined dramatically from 2012 to 2014. GEP declined more than TER and ET, leading to reduced carbon sequestration capacity and water use efficiency (WUE = GEP/ET). Neither annual nor growing-season precipitation could explain the year-to-year variations in carbon fluxes, whereas at our site ET was a better proxy for water available to ecosystem carbon exchange on an annual basis. Autumn soil moisture levels were carried over winter to the following spring, and, thus, may affect the rates of leafout, plant growth and carbon uptake in the early to mid-growing season. Our conclusions were drawn from only three years of measurements and are therefore preliminary. Longer timeseries encompassing a wider range of precipitation and soil moisture conditions are needed to confirm or refine these conclusions. Our findings highlight the importance of precipitation timing and soil moisture carry-over in controlling ecosystem productivity. Winter warming and decreases in autumn and winter precipitation may induce spring drought and thus impair the carbon sequestration potential of shrubland and steppe ecosystems in semi-arid and arid Eurasia. (C) 2016 Elsevier B.V. All rights reserved.


英文关键词Carbon balance Carry-over Eddy-covariance Inter-annual variability Soil water availability Water use efficiency
类型Article
语种英语
国家Peoples R China ; Finland
收录类别SCI-E
WOS记录号WOS:000383295200011
WOS关键词NET ECOSYSTEM EXCHANGE ; RAIN-USE EFFICIENCY ; CO2 EXCHANGE ; TERRESTRIAL ECOSYSTEMS ; NORTHERN CHINA ; CLIMATE-CHANGE ; FLUXES ; DROUGHT ; DESERT ; RESPIRATION
WOS类目Agronomy ; Forestry ; Meteorology & Atmospheric Sciences
WOS研究方向Agriculture ; Forestry ; Meteorology & Atmospheric Sciences
来源机构北京林业大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/191072
作者单位1.Beijing Forestry Univ, Sch Soil & Water Conservat, Yanchi Res Stn, Beijing 100083, Peoples R China;
2.Beijing Forestry Univ, Key Lab Soil & Water Conservat & Desertificat Com, Minist Educ, Beijing 100083, Peoples R China;
3.Univ Eastern Finland, Sch Forest Sci, Fac Sci & Forestry, Joensuu 80101, Finland
推荐引用方式
GB/T 7714
Jia, Xin,Zha, Tianshan,Gong, Jinnan,et al. Carbon and water exchange over a temperate semi-arid shrubland during three years of contrasting precipitation and soil moisture patterns[J]. 北京林业大学,2016,228:120-129.
APA Jia, Xin.,Zha, Tianshan.,Gong, Jinnan.,Wang, Ben.,Zhang, Yuqing.,...&Peltola, Hell.(2016).Carbon and water exchange over a temperate semi-arid shrubland during three years of contrasting precipitation and soil moisture patterns.AGRICULTURAL AND FOREST METEOROLOGY,228,120-129.
MLA Jia, Xin,et al."Carbon and water exchange over a temperate semi-arid shrubland during three years of contrasting precipitation and soil moisture patterns".AGRICULTURAL AND FOREST METEOROLOGY 228(2016):120-129.
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