参数的不确定性主导了21世纪巴西大部分地区的c周期预测误差

T. Smallman, D. Milodowski, E. S. Neto, Gerbrand Koren, J. Ometto, M. Williams
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引用次数: 7

摘要

摘要陆地碳(C)源和汇的识别对于了解地球系统以及减缓和适应温室气体排放导致的气候变化至关重要。利用陆地生态系统模式(TEMs)预测某一地点将作为碳源还是碳汇是具有挑战性的,因为净通量是具有很大不确定性的大得多的空间和时间可变通量之间的差。对政策评估至关重要的未来动态预测的不确定性,已通过对各种排放情景的多瞬变电磁法相互比较确定。这种方法量化了结构和受力误差。然而,参数误差在模型中的作用尚未确定。术语通常定义了从文献中生成的特定植物功能类型的参数。为了确定参数误差在预测中的重要性,我们提出了一种贝叶斯分析方法,利用巴西历史和当前的气温循环数据,对5个复杂程度不同的热变量进行参数化,并在1°空间分辨率下检索模型误差协方差。在对2001-2017年的数据进行评估后,在四种气候变化情景下,对参数化模式进行了至2100年的模拟,这些情景跨越了气候预估的可能范围。使用多个模型,每个模型具有每像素参数集合,我们划分预测不确定性。在模拟生物量C和死有机质(DOM)未来储量变化时,参数不确定性在巴西大部分地区占主导地位。模拟生物量变化的不确定性与木材的净初级生产力分配(NPPwood)和木材的平均停留时间(MRTwood)相关性最强。模拟DOM变化的不确定性与MRTsoil和nppwood相关性最强。由于这些变量和碳储量动态之间的耦合是双向的,我们认为使用木质生物量的重复估计将为改进未来碳循环的预测提供有价值的约束。最后,对我们的多模型分析的评估表明,木材凋落物对火灾排放有很大贡献,因此需要比大规模tem中通常考虑的更深入地了解木材凋落物C循环。
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Parameter uncertainty dominates C-cycle forecast errors over most of Brazil for the 21st century
Abstract. Identification of terrestrial carbon (C) sources and sinks is critical for understanding the Earth system as well as mitigating and adapting to climate change resulting from greenhouse gas emissions. Predicting whether a given location will act as a C source or sink using terrestrial ecosystem models (TEMs) is challenging due to net flux being the difference between far larger, spatially and temporally variable fluxes with large uncertainties. Uncertainty in projections of future dynamics, critical for policy evaluation, has been determined using multi-TEM intercomparisons, for various emissions scenarios. This approach quantifies structural and forcing errors. However, the role of parameter error within models has not been determined. TEMs typically have defined parameters for specific plant functional types generated from the literature. To ascertain the importance of parameter error in forecasts, we present a Bayesian analysis that uses data on historical and current C cycling for Brazil to parameterise five TEMs of varied complexity with a retrieval of model error covariance at 1∘ spatial resolution. After evaluation against data from 2001–2017, the parameterised models are simulated to 2100 under four climate change scenarios spanning the likely range of climate projections. Using multiple models, each with per pixel parameter ensembles, we partition forecast uncertainties. Parameter uncertainty dominates across most of Brazil when simulating future stock changes in biomass C and dead organic matter (DOM). Uncertainty of simulated biomass change is most strongly correlated with net primary productivity allocation to wood (NPPwood) and mean residence time of wood (MRTwood). Uncertainty of simulated DOM change is most strongly correlated with MRTsoil and NPPwood. Due to the coupling between these variables and C stock dynamics being bi-directional, we argue that using repeat estimates of woody biomass will provide a valuable constraint needed to refine predictions of the future carbon cycle. Finally, evaluation of our multi-model analysis shows that wood litter contributes substantially to fire emissions, necessitating a greater understanding of wood litter C cycling than is typically considered in large-scale TEMs.
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