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Photosynthesis drives anomalies in net carbon-exchange of pine forests at different latitudes

机译:光合作用驱动不同纬度的松树林净碳交换异常

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The growth rate of atmospheric CO2 exhibits large temporal variation that is largely determined by year-to-year fluctuations in land-atmosphere CO2 fluxes. This land-atmosphere CO2-flux is driven by large-scale biomass burning and variation in net ecosystem exchange (NEE). Between- and within years, NEE varies due to fluctuations in climate. Studies on climatic influences on inter- and intra-annual variability in gross photosynthesis (GPP) and net carbon uptake in terrestrial ecosystems have shown conflicting results. These conflicts are in part related to differences in methodology and in part to the limited duration of some studies. Here, we introduce an observation-driven methodology that provides insight into the dependence of anomalies in CO2 fluxes on climatic conditions. The methodology was applied on fluxes from a boreal and two temperate pine forests. Annual anomalies in NEE were dominated by anomalies in GPP, which in turn were correlated with incident radiation and vapor pressure deficit (VPD). At all three sites positive anomalies in NEE (a reduced uptake or a stronger source than the daily sites specific long-term average) were observed on summer days characterized by low incident radiation, low VPD and high precipitation. Negative anomalies in NEE occurred mainly on summer days characterized by blue skies and mild temperatures. Our study clearly highlighted the need to use weather patterns rather than single climatic variables to understand anomalous CO2 fluxes. Temperature generally showed little direct effect on anomalies in NEE but became important when the mean daily air temperature exceeded 23 degrees C. On such days GPP decreased likely because VPD exceeded 2.0 kPa, inhibiting photosynthetic uptake. However, while GPP decreased, the high temperature stimulated respiration, resulting in positive anomalies in NEE. Climatic extremes in summer were more frequent and severe in the South than in the North, and had larger effects in the South because the criteria to inhibit photosynthesis are more often met.
机译:大气CO2的增长率呈现出较大的时间变化,这在很大程度上取决于陆地大气CO2通量的逐年波动。这种陆地-大气中的二氧化碳通量是由大规模生物质燃烧和净生态系统交换(NEE)的变化驱动的。在几年之间以及几年之内,NEE因气候波动而变化。气候变化对陆地生态系统总光合作用(GPP)和年净碳吸收的年际和年际变化的影响的研究显示出相互矛盾的结果。这些冲突部分与方法上的差异有关,部分与某些研究期限有限有关。在这里,我们介绍了一种观察驱动的方法,该方法提供了对二氧化碳通量异常对气候条件的依赖性的洞察力。该方法应用于来自北方和两个温带松树林的通量。 NEE中的年度异常主要由GPP中的异常控制,而GPP中的异常又与入射辐射和蒸气压赤字(VPD)相关。在夏季,观测到的所有事件中三个地点的NEE均呈正异常(摄取量减少或来源比长期特定地点的长期平均水平更高),其特征是入射辐射低,VPD低,降水高。 NEE的负异常主要发生在以蓝天和温和为特征的夏季。我们的研究明确强调需要使用天气模式而不是单个气候变量来了解异常的CO2通量。温度通常对NEE中的异常几乎没有直接影响,但是当日平均气温超过23摄氏度时就变得很重要。在这几天,GPP可能会下降,因为VPD超过2.0 kPa,抑制了光合吸收。但是,尽管GPP下降,但高温刺激了呼吸,导致NEE出现正异常。夏季的极端气候在南部比北部更频繁,更严重,并且在南部的影响更大,因为更经常满足抑制光合作用的标准。

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