Impact of Drought Stress on Net CO2 Exchange above an Alpine Grassland Ecosystem in the Central Tibetan Plateau

  • 1 Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China;
    2 University of Chinese Academy of Sciences, Beijing 100049, China

Received date: 2013-05-23

  Revised date: 2013-12-02

  Online published: 2013-12-20

Supported by

National Basic Research Program of China (No.2010CB833500), and National Natural Science Foundation of China (Grant No.41171044).


Drought may impact the net ecosystem exchange of CO2 (NEE) between grassland ecosystems and the atmosphere during growth seasons. Here, carbon dioxide exchange and controlling factors in alpine grassland under drought stress in the hinterland of Tibetan Plateau (Damxung, Tibet, China) were investigated. Data were obtained using the covariance eddy technique in 2009. Severe drought stress appeared in the early growing season (May to early July) and September. Drought conditions during the early growing season limited grass production and the green leaf area index (GLAI) increased slowly, with an obvious decline in June. When encountering severe water stress, diurnal patterns of NEE in the growth season altered with a peak carbon release around 16:00 h or a second carbon uptake period before sunset. NEE variations in daytime related most closely with θ other than PAR when daily averaged θ<0.1 m3 m-3. Seasonal patterns of gross primary production (GPP) and NEE were also influenced by drought: the maximum and minimum of daily-integrated NEE were 0.9 g C m-2 d-1 on 3 July 2009, and -1.3 g C m-2 d-1 on 12 August 2009 with a GPP peak (-2.3 g C m-2 d-1) on the same day, respectively. Monthly NEE from May to July remained as carbon release and increased gradually; peak values of monthly NEE and GPP both appeared in August, but that of ecosystem respiration (Reco) was reached in July. Annual NEE, GPP and Reco of the alpine grassland ecosystem were 52.4, -158.1 and 210.5 g C m-2, respectively. Therefore, the grassland was a moderate source of CO2 to the atmosphere in this dry year. Interannual variation in NEE was likely related to different water conditions in the growing season. The three greatest contributors to seasonal variation in NEE, GPP and Reco respectively were GLAI>Ta>θ, GLAI>θ>PPT, and Ta>GLAI>PAR. Seasonality of GLAI explained 60.7% and 76.1% of seasonal variation in NEE and GPP, respectively. GPP or NEE was more sensitive than Reco to variation in GLAI, and ecosystem water conditions.

Cite this article

ZHAO Yuping, ZHANG Xianzhou, SHI Peili, WANG Jingsheng, WU Jianshuang . Impact of Drought Stress on Net CO2 Exchange above an Alpine Grassland Ecosystem in the Central Tibetan Plateau[J]. Journal of Resources and Ecology, 2013 , 4(4) : 327 -336 . DOI: 10.5814/j.issn.1674-764x.2013.04.005


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