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Parameter-state ensemble thinning for short-term hydrological prediction

机译:用于短期水文预测的参数 - 状态整体稀疏

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摘要

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 km(2)) 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:水文建模中的主要不确定性源可以概括为结构错误,参数错误和数据错误。操作系统莫德尔斯通常更关注预测能力而不是模型误差,本文提出了一种提高预测能力的新简单方法。该方法称为参数 - 状态集合变薄(P集)。 P-Set采用连续模型的大型集合运行,并应用筛选标准以减少集合的大小。目标是在预测期间找到最有前途的参数状态用于分析的组合。每个预测时段以相同的大型集合开始,但是筛选标准可以自由地为每个单独的预测时段选择不同的模拟子集。案例研究于2014年6月至2014年10月,仅限于加拿大安大略省湖北部的小型(1324公里(2))分水岭,采用加拿大半分布的水文陆地面积方案。该研究审查了这种方法在数据中的各种级别的工作程度如何,在流出和降水中开始,在流出和降水中开始,然后在沉淀中的流流和确定性中的不确定性,最后在流流流程和降水中的不确定性。当流出和降水相当确定时,发现该方法在这种情况下工作,同时在未来流流和降水的预测场景中实现更具挑战性,而是在未来的流流和降水的情况下不太确定。讨论了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。该方法还突出了模型结构误差,也讨论过。

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