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Ensemble Kalman filter data assimilation for a process-based catchment scale model of surface and subsurface flow

机译:基于过程和集水规模的地表和地下流的集合卡尔曼滤波数据同化

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摘要

A sequential data assimilation procedure based on the ensemble Kalman filter (EnKF) is introduced and tested for a process-based numerical model of coupled surface and subsurface flow. The model is based on the three-dimensional Richards equation for variably saturated porous media and a diffusion wave approximation for overland and channel flow. A one-dimensional soil column experiment and a three-dimensional tilted v-catchment test case are presented. A preliminary analysis of the assimilation scheme is undertaken for the one-dimensional test case in order to validate the implementation by comparison with published results and to assess the influence of various factors on the filter's performance. The numerical results suggest robustness with respect to the ensemble size and provide useful information for the more complex tilted v-catchment test case. The assimilation frequency and the effects induced by data assimilation on the surface and/or subsurface system states are then evaluated for the v-catchment experiment using synthetic observations of pressure head and streamflow. The results suggest that streamflow prediction can be improved by assimilation of pressure head and streamflow, either individually or in tandem, whereas assimilation of streamflow data alone does not improve the subsurface system state. In terms of the global system state, i.e., surface and subsurface variables, frequent updates are especially beneficial when assimilating both pressure head and streamflow. Furthermore, it is shown that better evaluation of the subsurface volume resulting from assimilation of head data is crucial for improving subsequent surface response.
机译:引入了基于集合卡尔曼滤波器(EnKF)的顺序数据同化程序,并进行了测试,以建立基于过程的表面和地下流动耦合的数值模型。该模型基于可变饱和多孔介质的三维Richards方程以及陆上和河道流动的扩散波近似。提出了一个一维土柱实验和一个三维倾斜V形集水试验案例。对一维测试用例进行了同化方案的初步分析,以便通过与已发布的结果进行比较来验证实现,并评估各种因素对滤波器性能的影响。数值结果表明了整体大小的鲁棒性,并为更复杂的倾斜v形集水测试案例提供了有用的信息。然后,使用压力头和水流的综合观测结果,对垂直集水实验评估同化频率和数据同化对表面和/或地下系统状态引起的影响。结果表明,通过单独或串联吸收压力头和流量可以改善流量预测,而仅吸收流量数据并不能改善地下系统状态。就整体系统状态(即地表和地下变量)而言,当同时吸收压头和水流时,频繁更新尤其有益。此外,已表明,更好地评估由头部数据同化产生的地下体积对于改善后续的表面响应至关重要。

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