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20th century changes in carbon isotopes and water-use efficiency: tree-ring-based evaluation of the CLM4.5 and LPX-Bern models

机译:20世纪碳同位素的变化和水利用效率:CLM4.5和LPX-BERN模型的树木为基础的评价

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Measurements of the stable carbon isotope ratio (delta C-13) on annual tree rings offer new opportunities to evaluate mechanisms of variations in photosynthesis and stomatal conductance under changing CO2 and climate conditions, especially in conjunction with process-based biogeochemical model simulations. The isotopic discrimination is indicative of the ratio between the CO2 partial pressure in the intercellular cavities and the atmosphere (c(i)/c(a)) and of the ratio of assimilation to stomatal conductance, termed intrinsic water-use efficiency (iWUE). We performed isotope-enabled simulations over the industrial period with the land biosphere module (CLM4.5) of the Community Earth System Model and the Land Surface Processes and Exchanges (LPX-Bern) dynamic global vegetation model. Results for C3 tree species show good agreement with a global compilation of delta C-13 measurements on leaves, though modeled C-13 discrimination by C3 trees is smaller in arid regions than measured. A compilation of 76 tree-ring records, mainly from Europe, boreal Asia, and western North America, suggests on average small 20th century changes in isotopic discrimination and in c(i)/c(a) and an increase in iWUE of about 27% since 1900. LPX-Bern results match these century-scale reconstructions, supporting the idea that the physiology of stomata has evolved to optimize trade-offs between carbon gain by assimilation and water loss by transpiration. In contrast, CLM4.5 simulates an increase in discrimination and in turn a change in iWUE that is almost twice as large as that revealed by the tree-ring data. Factorial simulations show that these changes are mainly in response to rising atmospheric CO2. The results suggest that the downregulation of c(i)/c(a) and of photosynthesis by nitrogen limitation is possibly too strong in the standard setup of CLM4.5 or that there may be problems associated with the implementation of conductance, assimilation, and related adjustment processes on long-term environmental changes.
机译:在一年生树木年轮上测量稳定碳同位素比值(δC-13)提供了新的机会来评估在变化的二氧化碳和气候条件下光合作用和气孔导度的变化机制,尤其是结合基于过程的生物地球化学模型模拟。同位素鉴别表明细胞间腔和大气中的CO2分压之比(c(i)/c(a))以及同化与气孔导度之比,称为内在水分利用效率(iWUE)。我们使用社区地球系统模型的陆地生物圈模块(CLM4.5)和陆地表面过程与交换(LPX-Bern)动态全球植被模型,在工业时期进行了同位素模拟。C3树种的结果与叶上delta C-13测量值的全球汇编显示出良好的一致性,尽管干旱地区C3树种的C-13识别模型小于测量值。一份主要来自欧洲、亚洲北部和北美西部的76份树木年轮记录的汇编表明,自1900年以来,20世纪同位素鉴别和c(i)/c(A)的平均变化较小,iWUE的增加约为27%。LPX-Bern的结果与这些百年尺度的重建相吻合,支持气孔生理学已经进化到优化同化碳增益和蒸腾水分损失之间的权衡的观点。相比之下,CLM4。5模拟了辨别力的增加,而iWUE的变化几乎是树轮数据显示的变化的两倍。阶乘模拟表明,这些变化主要是对大气CO2浓度上升的响应。结果表明,在CLM4的标准设置中,氮限制对c(i)/c(a)和光合作用的下调可能太强。5或在长期环境变化的传导、同化和相关调整过程中可能存在相关问题。

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