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Benchmarking NLDAS-2 Soil Moisture and Evapotranspiration to Separate Uncertainty Contributions

机译:对NLDAS-2土壤湿度和蒸散量进行基准分析以区分不确定性因素

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摘要

Model benchmarking allows us to separate uncertainty in model predictions caused by model inputs from uncertainty due to model structural error. We extend this method with a “large-sample” approach (using data from multiple field sites) to measure prediction uncertainty caused by errors in (i) forcing data, (ii) model parameters, and (iii) model structure, and use it to compare the efficiency of soil moisture state and evapotranspiration flux predictions made by the four land surface models in the North American Land Data Assimilation System Phase 2 (NLDAS-2). Parameters dominated uncertainty in soil moisture estimates and forcing data dominated uncertainty in evapotranspiration estimates; however, the models themselves used only a fraction of the information available to them. This means that there is significant potential to improve all three components of the NLDAS-2 system. In particular, continued work toward refining the parameter maps and look-up tables, the forcing data measurement and processing, and also the land surface models themselves, has potential to result in improved estimates of surface mass and energy balances.
机译:通过模型基准测试,我们可以将模型输入引起的模型预测不确定性与模型结构误差导致的不确定性区分开。我们使用“大样本”方法(使用来自多个野外站点的数据)扩展该方法,以测量由于(i)强制数据,(ii)模型参数和(iii)模型结构中的错误而导致的预测不确定性,并使用它比较北美土地数据同化系统第2阶段(NLDAS-2)的四个陆地表面模型得出的土壤水分状态和蒸散通量预测的效率。参数主导着土壤水分估算的不确定性,而强迫数据主导着蒸散估算的不确定性;但是,模型本身仅使用了一部分可用信息。这意味着有很大的潜力来改进NLDAS-2系统的所有三个组件。特别是,继续完善参数图和查找表,强制数据的测量和处理以及地面模型本身,都有可能改善对表面质量和能量平衡的估计。

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