Hawkesbury Institute for the Environment, Western Sydney University, Locked Bag 1797, Penrith, NSW, 2751, Australia.
Department of Biological Sciences, Macquarie University, North Ryde, NSW, 2109, Australia.
Glob Chang Biol. 2016 Aug;22(8):2834-51. doi: 10.1111/gcb.13268. Epub 2016 May 9.
The response of terrestrial ecosystems to rising atmospheric CO2 concentration (Ca ), particularly under nutrient-limited conditions, is a major uncertainty in Earth System models. The Eucalyptus Free-Air CO2 Enrichment (EucFACE) experiment, recently established in a nutrient- and water-limited woodland presents a unique opportunity to address this uncertainty, but can best do so if key model uncertainties have been identified in advance. We applied seven vegetation models, which have previously been comprehensively assessed against earlier forest FACE experiments, to simulate a priori possible outcomes from EucFACE. Our goals were to provide quantitative projections against which to evaluate data as they are collected, and to identify key measurements that should be made in the experiment to allow discrimination among alternative model assumptions in a postexperiment model intercomparison. Simulated responses of annual net primary productivity (NPP) to elevated Ca ranged from 0.5 to 25% across models. The simulated reduction of NPP during a low-rainfall year also varied widely, from 24 to 70%. Key processes where assumptions caused disagreement among models included nutrient limitations to growth; feedbacks to nutrient uptake; autotrophic respiration; and the impact of low soil moisture availability on plant processes. Knowledge of the causes of variation among models is now guiding data collection in the experiment, with the expectation that the experimental data can optimally inform future model improvements.
陆地生态系统对大气 CO2 浓度(Ca )升高的响应,特别是在养分有限的条件下,是地球系统模型中的一个主要不确定性因素。最近在养分和水分有限的林地中建立的桉树自由空气 CO2 富集(EucFACE)实验为解决这一不确定性提供了一个独特的机会,但如果能事先确定关键模型不确定性,则可以更好地实现这一目标。我们应用了七种植被模型,这些模型之前已经过全面评估,以模拟 EucFACE 可能出现的预先设定结果。我们的目标是提供定量预测,以便在数据收集时进行评估,并确定实验中应进行的关键测量,以便在实验后模型比较中区分替代模型假设。模拟的年净初级生产力(NPP)对升高的 Ca 的响应在模型间的范围从 0.5%到 25%不等。在低降雨年,NPP 的模拟减少也变化很大,从 24%到 70%不等。导致模型间出现分歧的关键过程包括生长的养分限制;养分吸收的反馈;自养呼吸;以及低土壤水分可用性对植物过程的影响。现在,对模型间差异的原因的了解正在指导实验中的数据收集,期望实验数据能够最佳地为未来的模型改进提供信息。