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Parameter-state ensemble thinning for short-term hydrological prediction

机译:短期水文预测的参数状态集成化

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The main sources of uncertainty in hydrological modelling can be summarized as structural errors, parameter errors, and data errors. Operational modellers are generally more concerned with predictive ability than model errors, and this paper presents a new, simple method to improve predictive ability. The method is called parameter-state ensemble thinning?(P-SET). P-SET takes a large ensemble of continuous model runs and applies screening criteria to reduce the size of the ensemble. The goal is to find the most promising parameter-state combinations for analysis during the prediction period. Each prediction period begins with the same large ensemble, but the screening criteria are free to select a different sub-set of simulations for each separate prediction period. The case study is from June to October?2014 for a small (1324?kmsup2/sup) watershed just north of Lake Superior in Ontario, Canada, using a Canadian semi-distributed hydrologic land-surface scheme. The study examines how well the approach works given various levels of certainty in the data, beginning with certainty in the streamflow and precipitation, followed by uncertainty in the streamflow and certainty in the precipitation, and finally uncertainty in both the streamflow and precipitation. The approach is found to work in this case when streamflow and precipitation are fairly certain, while being more challenging to implement in a forecasting scenario where future streamflow and precipitation are much less certain. The main challenge is determined to be related to parametric uncertainty and ideas for overcoming this challenge are discussed. The approach also highlights model structural errors, which are also discussed.
机译:水文模型不确定性的主要来源可以概括为结构误差,参数误差和数据误差。操作建模人员通常比模型错误更关注预测能力,本文提出了一种提高预测能力的简单方法。该方法称为参数状态集成细化(P-SET)。 P-SET包含大量连续模型运行的集合,并应用筛选标准以减小集合的大小。目标是找到最有希望的参数状态组合,以便在预测期间进行分析。每个预测周期都以相同的大集合开始,但是筛选标准可以为每个单独的预测周期自由选择不同的模拟子集。案例研究是从2014年6月至2014年10月,使用加拿大半分布式水文陆地表层计划,在加拿大安大略省苏必利尔湖以北的一个小(1324?km 2 )流域。这项研究研究了在给定数据的各种确定性级别后,该方法的效果如何,首先是流量和降水的确定性,然后是流量的不确定性和降水的确定性,最后是流量和降水的不确定性。在相当确定流量和降水的情况下,该方法适用于这种情况,而在未来流量和降水的不确定性更高的预测方案中,实施该方法更具挑战性。确定主要挑战与参数不确定性有关,并讨论了克服这一挑战的想法。该方法还突出显示了模型结构错误,对此也进行了讨论。

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