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Partitioning Climatic and Biotic Effects on Interannual Variability of Ecosystem Carbon Exchange in Three Ecosystems

机译:气候和生物效应对三种生态系统中碳交换的年际变化的分区效应

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Understanding the climatic and biotic controls of interannual variability (IAV) in net ecosystem exchange (NEE) is important for projecting future uptake of CO2 in terrestrial ecosystems. In this study, a statistical modeling approach was used to partition climatic and biotic effects on the IAV in NEE, gross primary productivity (GPP) and ecosystem respiration (RE) at a subtropical evergreen plantation in China (QYZ), a deciduous forest (MOZ), and a grassland (DK1) in the USA. The climatic effects in the study are defined as the interannual anomalies in carbon (C) fluxes directly caused by climatic variations, whereas the biotic effects are those caused by the IAV in photosynthetic and respiratory traits. The results showed that the contribution of biotic effects to the IAV in NEE increased significantly as the temporal scale got longer from daily to annual scales. At the annual scale, the contribution of biotic effects to the IAV in NEE was 47, 69, and 77% at QYZ, MOZ, and DK1, respectively. However, the IAV in NEE was mainly controlled by GPP at QYZ, and by RE at DK1, whereas the contributions of GPP and RE to the IAV in NEE were similar at MOZ, indicating different mechanisms regulating the IAV in NEE among ecosystems. Interestingly, there was a strong negative correlation between the climatic and biotic effects at the annual scale from 2003 to 2009 at QYZ (r(2) = 0.80, P 0.01), suggesting these two effects counteracted each other and resulted in a relatively stable C sink, whereas no correlations were found at the other two sites. Overall, our study revealed the relative importance of climatic and biotic effects on the IAV in NEE and contributed to our understanding of their underlying mechanisms.
机译:了解净生态系统交换(NEE)中年际变化(IAV)的气候和生物控制对于预测未来陆上生态系统中的CO2吸收非常重要。在这项研究中,采用统计建模方法对中国亚热带常绿人工林(QYZ),落叶林(MOZ)的NEE,总初级生产力(GPP)和生态系统呼吸(RE)的IAV的气候和生物影响进行分区。 )和美国的草原(DK1)。研究中的气候影响被定义为由气候变化直接引起的碳(C)通量的年际异常,而生物影响是由IAV在光合和呼吸性状上引起的。结果表明,随着时间尺度从日尺度到年尺度变长,生物效应对NEE中IAV的贡献显着增加。在年尺度上,QYZ,MOZ和DK1的生物效应对NEE中IAV的贡献分别为47%,69%和77%。但是,NEE中的IAV主要由QYZ的GPP和DK1中的RE所控制,而GPP和RE对NEE中的IAV的贡献在MOZ上相似,表明生态系统之间调节NEE中的IAV的机制不同。有趣的是,在2003年至2009年QYZ期间,气候效应和生物效应之间存在强烈的负相关性(r(2)= 0.80,P <0.01),这表明这两种效应相互抵消并导致相对稳定C下沉,而在其他两个位置未发现相关性。总体而言,我们的研究揭示了NEE中IAV的气候和生物影响的相对重要性,并有助于我们了解其潜在机制。

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