Charles B. Gauthier, Joe R. Melton, Gesa Meyer, S. N. Raj Deepak, Oliver Sonnentag
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引用次数: 0
Abstract
Accurate simulation of soil organic carbon (SOC) dynamics by terrestrial biosphere models is hampered by poorly constrained parameters and parameter equifinality, amongst other issues. To address this, we use Bayesian optimization to constrain the 16 SOC-related parameters in the Canadian Land Surface Scheme Including biogeochemical Cycles (CLASSIC). We employed a global sensitivity analysis (Sobol’) to develop four parameter sets based upon different sensitivity criteria. We then optimized each set against observed SOC (World Soil Information Service; WoSIS) and soil respiration (Soil Respiration Database; SRDB). Using two different loss functions; one focused on reproducing the observational mean value, and the other explicitly accounting for an estimated observational uncertainty. The best optimized parameter sets for each loss function had an average relative difference of 61%. Thus, the choice of loss function impacts what parameter values are deemed optimal and should be considered carefully. The final set of selected optimal parameters saw a 12% improvement against WoSIS and SRDB, had global SOC totals in line with literature estimates, and better simulated high-latitude SOC stocks evaluated against the Northern Circumpolar Soil Carbon Database (RMSD: 16.39 vs. 17.61; bias: −5.57 vs. −10.78 kg C ) compared to the default CLASSIC parameters. However, some parameters were not well constrained, in particular those of needle-leaf deciduous trees that dominate the Siberian boreal forests, a region relatively poorly observed in WoSIS and SRDB. Future work should apply further constraints on the optimization framework and address observational gaps.
陆地生物圈模型对土壤有机碳(SOC)动态的精确模拟受到参数约束不佳和参数等价性等问题的阻碍。为了解决这个问题,我们使用贝叶斯优化来约束加拿大陆地表面方案包括生物地球化学循环(CLASSIC)中的16个soc相关参数。我们采用全局敏感性分析(Sobol’),根据不同的敏感性标准制定了四个参数集。然后,我们根据观察到的SOC(世界土壤信息服务;WoSIS)和土壤呼吸(土壤呼吸数据库;SRDB)对每个集合进行优化。采用两种不同的损失函数;一种方法侧重于再现观测平均值,另一种方法明确地解释了估计的观测不确定性。每个损失函数的最佳优化参数集的平均相对差为61%。因此,损失函数的选择影响到哪些参数值被认为是最优的,需要仔细考虑。与WoSIS和SRDB相比,最终选择的最优参数集提高了12%,全球有机碳总量与文献估计一致,并且更好地模拟了北环极土壤碳数据库评估的高纬度有机碳储量(RMSD: 16.39 vs. 17.61;偏差:−5.57 vs.−10.78 kg C m−2 ${\mathrm{m}}^{-2}$)与默认的CLASSIC参数相比。然而,一些参数没有得到很好的约束,特别是在西伯利亚寒带森林中占主导地位的针叶落叶乔木的参数,这一区域在wsis和SRDB中观测相对较少。未来的工作应进一步限制优化框架,并解决观测差距。
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