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Neural error regression diagnosis (NERD): A tool for model bias identification and prognostic data assimilation

机译:神经错误回归诊断(NERD):用于模型偏差识别和预后数据同化的工具

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摘要

Data assimilation in the field of predictive land Surface modeling is generally limited to using observational data to estimate optimal model states or restrict model parameter ranges. To date, very little work has attempted to systematically define and quantify error resulting from a model's inherent inability to Simulate the natural system. This paper introduces a data assimilation technique that moves toward this goal by accounting for those deficiencies in the model itself that lead to systematic errors in model output. This is done using a supervised artificial neural network to "learn" and simulate systematic trends in the model output error. These simulations in turn are used to correct the model's output each time step. The technique is applied in two case studies, using fluxes of latent heat flux at one site and net ecosystem exchange (NEE) of carbon dioxide at another. Root-mean-square error (rmse) in latent heat flux per time step was reduced from 27.5 to 18.6 W m(-2) (32%) and monthly front 9.91 to 3.08 W m(-2) (68%). For NEE, rmse per time step was reduced front 3.71 to 2.70 mu mol m(-2) s(-1) (27%) and annually front 2.24 to 0.11 mu mol m(-2) s(-1) (95%). In both cases the correction provided significantly greater gains than single criteria parameter estimation on the same flux.
机译:预测性陆地领域中的数据同化地表建模通常限于使用观测数据来估计最佳模型状态或限制模型参数范围。迄今为止,很少有工作试图系统地定义和量化由于模型固有的无法模拟自然系统而导致的误差。本文介绍了一种数据同化技术,它通过考虑导致模型输出系统错误的模型本身的缺陷,朝着这个目标迈进。这是通过使用监督的人工神经网络来“学习”并模拟模型输出误差中的系统趋势来完成的。这些仿真依次用于校正每个时间步长的模型输出。该技术在两个案例研究中得到了应用,一个站点使用潜热通量,另一个站点使用二氧化碳的净生态系统交换(NEE)。每个时间步的潜热通量的均方根误差(rmse)从27.5降低到18.6 W m(-2)(32%),每月前沿从9.91降低到3.08 W m(-2)(68%)。对于NEE,每个时间步的均方根值降低到3.71到2.70μmolmol m(-2)s(-1)(27%)和每年2.24到0.11μmolmol m(-2)s(-1)(95%) )。在这两种情况下,与相同通量下的单个标准参数估计相比,校正提供的增益要大得多。

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