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Carbon and Water Use Efficiencies: A Comparative Analysis of Ten Terrestrial Ecosystem Models under Changing Climate

机译:碳和水的利用效率:气候变化下十种陆地生态系统模型的比较分析

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摘要

Terrestrial ecosystems carbon and water cycles are tightly coupled through photosynthesis and evapotranspiration processes. The ratios of carbon stored to carbon uptake and water loss to carbon gain are key ecophysiological indicators essential to assess the magnitude and response of the terrestrial plant to the changing climate. Here, we use estimates from 10 terrestrial ecosystem models to quantify the impacts of climate, atmospheric CO2 concentration, and nitrogen (N) deposition on water use efficiency (WUE), and carbon use efficiency (CUE). We find that across models, WUE increases over the 20th Century particularly due to CO2 fertilization and N deposition and compares favorably to experimental studies. Also, the results show a decrease in WUE with climate for the last 3 decades, in contrasts with up-scaled flux observations that demonstrate a constant WUE. Modeled WUE responds minimally to climate with modeled CUE exhibiting no clear trend across space and time. The divergence between simulated and observationally-constrained WUE and CUE is driven by modeled NPP and autotrophic respiration, nitrogen cycle, carbon allocation, and soil moisture dynamics in current ecosystem models. We suggest that carbon-modeling community needs to reexamine stomatal conductance schemes and the soil-vegetation interactions for more robust modeling of carbon and water cycles.
机译:陆地生态系统的碳和水循环通过光合作用和蒸散过程紧密耦合。碳存储量与碳吸收量的比值以及水分损失与碳吸收量的比值是关键的生态生理指标,对于评估陆生植物对气候变化的幅度和响应至关重要。在这里,我们使用来自10个陆地生态系统模型的估计值来量化气候,大气中的CO2浓度和氮(N)沉积对水利用效率(WUE)和碳利用效率(CUE)的影响。我们发现,在所有模型中,WUE在20世纪都增加了,特别是由于CO2施肥和N沉积所致,并且与实验研究相比具有优势。而且,结果表明,过去三十年来,随着气候的变化,WUE有所降低,这与大规模的通量观测结果相反,表明WUE不变。模拟的WUE对气候的响应最小,模拟的CUE在时空上没有明显的趋势。在当前的生态系统模型中,模拟的NPP和自养呼吸,氮循环,碳分配和土壤水分动力学驱动了模拟的WEE和受观测约束的WUE和CUE之间的差异。我们建议碳模型界需要重新审查气孔导度方案和土壤-植被相互作用,以建立更健壮的碳和水循环模型。

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