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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世纪碳同位素和水利用效率的变化:基于树环的CLM4.5和LPX-Bern模型评估

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摘要

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(δC-13)提供了新的机会来评估在不断变化的CO2和气候条件下光合作用和气孔导度变化的机制,尤其是结合基于过程的生物地球化学模型模拟。同位素判别指示细胞间腔和大气中的CO2分压之比(c(i)/ c(a))和同化与气孔导度之比,称为固有用水效率(iWUE) 。我们使用社区地球系统模型的陆地生物圈模块(CLM4.5)和地球表面过程与交换(LPX-Bern)动态全球植被模型在工业期间进行了基于同位素的模拟。 C3树种的结果与叶子上的C-13增量测量的总体汇编显示出很好的一致性,尽管在干旱地区C3树对C-13的建模判别比测量的小。汇集了76个主要来自欧洲,北亚和北美洲西部的树年轮记录,表明20世纪同位素歧视和c(i)/ c(a)的平均变化很小,而iWUE值增加了约27自1900年以来的百分比。LPX-Bern的结果与这些世纪规模的重建相吻合,支持了这样的观点,即气孔的生理学已经发展到可以优化吸收同化碳与蒸腾水分之间的权衡。相反,CLM4.5模拟了辨别力的增加,而iWUE的改变几乎是树环数据揭示的两倍。析因仿真表明,这些变化主要是由于大气中CO2的升高所致。结果表明,在CLM4.5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,或者可能与电导,同化和有关长期环境变化的相关调整过程。

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