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碳和水利用效率:十种陆地生态系统模型在气候变化下的比较分析。

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

机构信息

Department of Earth and Environmental Sciences, Murray State University, Murray, KY, 42071, USA.

Woods Hole Research Center, Falmouth, MA, 02540, USA.

出版信息

Sci Rep. 2019 Oct 11;9(1):14680. doi: 10.1038/s41598-019-50808-7.

DOI:10.1038/s41598-019-50808-7
PMID:31604972
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6789101/
Abstract

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 CO concentration, and nitrogen (N) deposition on water use efficiency (WUE), and carbon use efficiency (CUE). We find that across models, WUE increases over the 20 Century particularly due to CO 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.

摘要

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。碳存储与碳吸收、水分损失与碳增益的比值是评估陆地植物对气候变化的幅度和响应的关键生理生态指标。在这里,我们使用 10 个陆地生态系统模型的估计值来量化气候、大气 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,在整个模型中,WUE 在 20 世纪增加,特别是由于 CO2 施肥和 N 沉积,与实验研究相比表现良好。此外,结果表明,在过去的 30 年中,WUE 随着气候的变化而减少,与放大通量观测形成对比,后者表明 WUE 保持不变。模型化的 WUE 对气候的响应很小,而模型化的 CUE 在空间和时间上没有明显的趋势。模拟和观测约束的 WUE 和 CUE 之间的差异是由当前生态系统模型中的模型化 NPP 和自养呼吸、氮循环、碳分配和土壤湿度动态驱动的。我们建议,碳建模界需要重新审视气孔导度方案和土壤-植被相互作用,以更稳健地模拟碳和水循环。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/88b6/6789101/ef39306e4f76/41598_2019_50808_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/88b6/6789101/33fb7a7596a3/41598_2019_50808_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/88b6/6789101/b47d38f9e9f6/41598_2019_50808_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/88b6/6789101/68bda9a9a864/41598_2019_50808_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/88b6/6789101/ef39306e4f76/41598_2019_50808_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/88b6/6789101/33fb7a7596a3/41598_2019_50808_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/88b6/6789101/b47d38f9e9f6/41598_2019_50808_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/88b6/6789101/68bda9a9a864/41598_2019_50808_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/88b6/6789101/ef39306e4f76/41598_2019_50808_Fig4_HTML.jpg

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Uncertainty in the response of terrestrial carbon sink to environmental drivers undermines carbon-climate feedback predictions.
变暖抑制了印度植被净初级生产力的增长,尽管那里正在变绿。
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