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Median to Strong Rainfall Intensity Favors Carbon Sink in a Temperate Grassland Ecosystem in China

Author

Listed:
  • Guangcun Hao

    (School of Geography, South China Normal University, Guangzhou 510631, China)

  • Zhongmin Hu

    (School of Geography, South China Normal University, Guangzhou 510631, China
    Southern Marine Science and Engineering Guangdong Laboratory, Zhuhai 519082, China)

  • Qun Guo

    (Synthesis Research Center of Chinese Ecosystem Research Network, Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
    College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100190, China)

  • Kai Di

    (School of Geography, South China Normal University, Guangzhou 510631, China)

  • Shenggong Li

    (Synthesis Research Center of Chinese Ecosystem Research Network, Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
    College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100190, China)

Abstract

Over the past 50 years, rainfall events have made significant alterations to environments due to global warming. The grasslands in arid and semi-arid regions are extremely sensitive to variations in rainfall patterns, which are considered to significantly affect ecosystem functions. In this study, an experiment with varying rainfall sizes and frequencies (0 mm, 2 mm, 5 mm, 10 mm, 20 mm, and 40 mm) was conducted during growing seasons in typical grasslands, to study the effect of changes in rainfall regime on net ecosystem exchange (NEE). Our results indicated that NEE exhibited nonlinear responses to rainfall treatments, and reached its peak under 20 mm in middle growing season. Further, the component fluxes of both NEE (i.e., gross primary productivity (GPP)) and ecosystem respiration (ER) illustrated nonlinear responses to treatment gradient, with peak values at 20 mm and 5 mm, respectively. Based on five-year eddy flux measurements, further analyses demonstrated that GPP and ER increased with increasing soil moisture, and net ecosystem carbon uptake (-1*NEE) was significantly stimulated due to a more enhanced GPP than ER, when soil moisture was above 8%. Additionally, we found that the response of root biomass was different from that of carbon fluxes to changes in rainfall patterns. Overall, these findings highlight the importance of both changes in rainfall regimes in controlling ecosystem C exchange and investigation of the potential threshold for ecosystem function shifts, which are crucial to further understand C cycles in grasslands.

Suggested Citation

  • Guangcun Hao & Zhongmin Hu & Qun Guo & Kai Di & Shenggong Li, 2019. "Median to Strong Rainfall Intensity Favors Carbon Sink in a Temperate Grassland Ecosystem in China," Sustainability, MDPI, vol. 11(22), pages 1-13, November.
    • Handle: RePEc:gam:jsusta:v:11:y:2019:i:22:p:6376-:d:286479
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    References listed on IDEAS

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    1. Julia K. Green & Sonia I. Seneviratne & Alexis M. Berg & Kirsten L. Findell & Stefan Hagemann & David M. Lawrence & Pierre Gentine, 2019. "Large influence of soil moisture on long-term terrestrial carbon uptake," Nature, Nature, vol. 565(7740), pages 476-479, January.
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