A Bayesian consistent dual ensemble Kalman filter for state-parameter estimation in subsurface hydrology

被引:28
作者
Ait-El-Fquih, Boujemaa [1 ]
El Gharamti, Mohamad [1 ,2 ]
Hoteit, Ibrahim [1 ]
机构
[1] KAUST, Dept Earth Sci & Engn, Thuwal 239556900, Saudi Arabia
[2] NERSC, Mohn Sverdrup Ctr Global Ocean Studies & Operat O, N-5006 Bergen, Norway
关键词
STOCHASTIC MOMENT EQUATIONS; DATA ASSIMILATION; GROUNDWATER-FLOW; HYDRAULIC-CONDUCTIVITY; UNCERTAINTY ASSESSMENT; PARTICLE FILTER; SOIL-MOISTURE; MODEL; OPTIMIZATION; EVOLUTION;
D O I
10.5194/hess-20-3289-2016
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Ensemble Kalman filtering (EnKF) is an efficient approach to addressing uncertainties in subsurface ground-water models. The EnKF sequentially integrates field data into simulation models to obtain a better characterization of the model's state and parameters. These are generally estimated following joint and dual filtering strategies, in which, at each assimilation cycle, a forecast step by the model is followed by an update step with incoming observations. The joint EnKF directly updates the augmented state-parameter vector, whereas the dual EnKF empirically employs two separate filters, first estimating the parameters and then estimating the state based on the updated parameters. To develop a Bayesian consistent dual approach and improve the state-parameter estimates and their consistency, we propose in this paper a one-step-ahead (OSA) smoothing formulation of the state-parameter Bayesian filtering problem from which we derive a new dual-type EnKF, the dual EnKF(OSA). Compared with the standard dual EnKF, it imposes a new update step to the state, which is shown to enhance the performance of the dual approach with almost no increase in the computational cost. Numerical experiments are conducted with a two-dimensional (2-D) synthetic groundwater aquifer model to investigate the performance and robustness of the proposed dual EnKFOSA, and to evaluate its results against those of the joint and dual EnKFs. The proposed scheme is able to successfully recover both the hydraulic head and the aquifer conductivity, providing further reliable estimates of their uncertainties. Furthermore, it is found to be more robust to different assimilation settings, such as the spatial and temporal distribution of the observations, and the level of noise in the data. Based on our experimental setups, it yields up to 25% more accurate state and parameter estimations than the joint and dual approaches.
引用
收藏
页码:3289 / 3307
页数:19
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