文献类型： 外文期刊

作者： Jiang, Yan ¹ ; Wang, Peng ³ ; Xu, Xiangde ⁴ ; Zhang, Jiahua ⁵ ;

作者机构： 1.Shihezi Univ, Dept Resources & Environm Sci, Shihezi 832003, Xinjiang, Peoples R China

2.China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China

3.Xinjiang Acad Agr & Reclamat Sci, Inst Crop Res, Xinjiang 832000, Shihezi, Peoples R China

4.Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China

5.Chinese Acad Sci, Inst Remote Sensing & Digital Earth, Key Lab Digital Earth Sci, Beijing 100094, Peoples R China

关键词： Tibetan Plateau;Carbon source/sink;Carbon fluxes;Vegetation;Terrain;Meteorological factor

期刊名称：ENVIRONMENTAL EARTH SCIENCES （ 影响因子：2.784； 五年影响因子：2.867 ）

ISSN： 1866-6280

年卷期： 2014 年 72 卷 11 期

页码：

收录情况： SCI

摘要： Tibetan Plateau (TP) is the highest and most extensive plateau in the world and has been known as the roof of the world, and it is sensitive to climate change. The researches of CO2 fluxes (F (C)) in the TP region play a significant role in understanding regional and global carbon balance and climate change. Eddy covariance flux measurements were conducted at three sites of south-eastern TP comprising Dali (DL, cropland ecosystem), LinZhi (LZ, alpine meadow ecosystem) and Wenjiang (WJ, cropland ecosystem); amongst those DL and LZ are located in plateau region, while WJ is in plain region. Dynamics of F (C) and influences of vegetation, meteorological (air temperature, photosynthetically active radiation, soil temperature and soil water content) and terrain factors (altitude) were analysed on the basis of data taken during 2008. The results showed that, in the cool sub-season (March, April, October and December), carbon sink appeared even in December with fluxes of (-0.021 to -0.05) mg CO2 m(-2) s(-1) and carbon source only in October (0.03 +/- A 0.0048) mg CO2 m(-2) s(-1) in DL and WJ site. In LZ site, carbon sink was observed in April: (-0.036 +/- A 0.0023) mg CO2 m(-2) s(-1) and carbon sources in December and March (0.008-0.010 mg CO2 m(-2) s(-1)). In the hot sub-season (May-August), carbon source was observed only in May with (0.011 +/- A 0.0022), (0.104 +/- A 0.0029) and (0.036 +/- A 0.0017) fluxes in LZ, DL and WJ site, respectively, while carbon sinks with (-0.021 +/- A 0.0041), (-0.213 +/- A 0.0007) and (-0.110 +/- A 0.0015) mg CO2 m(-2) s(-1) fluxes in LZ, DL, and WJ, respectively. Comparing with plain region (WJ), carbon sinks in plateau region (DL and LZ) lasted for a longer time, and the absorption sum was large and up to (-357.718 +/- A 0.0054) and (-371.111 +/- A 0.0039) g C m(-2) year(-1), respectively. The LZ site had the weakest carbon sink with (-178.547 +/- A 0.0070) g C m(-2) year(-1). Multivariate analysis of covariance showed that altitude (AL) as an independent factor explained 39.5 % of F (C) (P < 0.026). F (C) had a quadratic relationship with Normalized difference vegetation index (NDVI) (R (2) ranges from 0.485 to 0.640 for three sites), an exponential relationship with soil temperature at 5-cm depth (ST (5)) at night time and a quadratic relationship with air temperature (T (a)) at day time. Path analysis indicated that photosynthetically active radiation (PAR), sensible heat fluxes (H) and other factors all had direct or indirect effects on F (C) in all of the three tested sites around the south-eastern TP.