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引用次数: 0
摘要
陆地生物圈模式通过整合不同尺度的生态过程,提供了全球碳循环的全面视角,但由于过程表示和参数变化的多样性,这些模式在气候和生物地球化学预测方面带来了很大的不确定性。例如,不同的土壤水分限制函数导致不同模型的生产力范围很大。为了解决这个问题,我们提出了可微分土地模型(DifferLand),这是一种新颖的混合机器学习方法,用神经网络(NN)代替模型中未知的水分限制函数,从数据中学习。利用自动差异化技术,我们根据对 16 个 FLUXNET 站点的蒸散量、总初级生产力、生态系统呼吸作用和叶面积指数的日常观测结果,校准了嵌入式神经网络和物理模型参数。我们根据测试数据集评估了六种模型配置,在这些配置中,NN 模拟了日益复杂的土壤水分与光合作用之间的相互作用,从而找到了结构与性能之间的最佳平衡点。我们的研究结果表明,采用单变量 NN 的简单混合模型能有效捕捉月度时间尺度上的站点水平水通量和碳通量。在全球干旱梯度上,水压力限制的程度各不相同,但其函数形式始终趋同于与高水位饱和度的片断线性关系。虽然包含更多土壤水和气象驱动因素之间相互作用的模型能更好地拟合更细时间尺度上的观测结果,但它们也存在过度拟合和等效性问题。我们的研究表明,混合模型在学习未知参数和检验生态假设方面具有巨大潜力。尽管如此,仍需根据观测限制因素谨慎权衡结构与性能,以便将检索到的关系转化为对过程的有力理解。
Exploring Optimal Complexity for Water Stress Representation in Terrestrial Carbon Models: A Hybrid-Machine Learning Model Approach
Terrestrial biosphere models offer a comprehensive view of the global carbon cycle by integrating ecological processes across scales, yet they introduce significant uncertainties in climate and biogeochemical projections due to diverse process representations and parameter variations. For instance, different soil water limitation functions lead to wide productivity ranges across models. To address this, we propose the Differentiable Land Model (DifferLand), a novel hybrid machine learning approach replacing unknown water limitation functions in models with neural networks (NNs) to learn from data. Using automatic differentiation, we calibrated the embedded NN and the physical model parameters against daily observations of evapotranspiration, gross primary productivity, ecosystem respiration, and leaf area index across 16 FLUXNET sites. We evaluated six model configurations where NNs simulate increasingly complex soil water and photosynthesis interactions against test data sets to find the optimal structure-performance tradeoff. Our findings show that a simple hybrid model with a univariate NN effectively captures site-level water and carbon fluxes on a monthly timescale. Across a global aridity gradient, the magnitude of water stress limitation varies, but its functional form consistently converges to a piecewise linear relationship with saturation at high water levels. While models incorporating more interactions between soil water and meteorological drivers better fit observations at finer time scales, they risk overfitting and equifinality issues. Our study demonstrates that hybrid models have great potential in learning unknown parameterizations and testing ecological hypotheses. Nevertheless, careful structure-performance tradeoffs are warranted in light of observational constraints to translate the retrieved relationships into robust process understanding.
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