Analysis of iterative ensemble smoothers for solving inverse problems

被引:140
作者
Evensen, Geir [1 ,2 ]
机构
[1] Int Res Inst Stavanger, Bergen, Norway
[2] Nansen Environm & Remote Sensing Ctr, Bergen, Norway
关键词
Ensemble smoothers; IES; ES-MDA; Data assimilation; History matching; DATA ASSIMILATION;
D O I
10.1007/s10596-018-9731-y
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
This paper examines the properties of the Iterated Ensemble Smoother (IES) and the Multiple Data Assimilation Ensemble Smoother (ES-MDA) for solving the history matching problem. The iterative methods are compared with the standard Ensemble Smoother (ES) to improve the understanding of the similarities and differences between them. We derive the three smoothers from Bayes' theorem for a scalar case which allows us to compare the equations solved by the three methods, and we can better understand which assumptions are applied and their consequences. When working with a scalar model, it is possible to use a vast ensemble size, and we can construct the sample distributions for both priors and posteriors, as well as intermediate iterates. For a linear model, all three methods give the same result. For a nonlinear model, the iterative methods improve on the ES result, but the two iterative methods converge to different solutions, and it is not clear which should be the preferred choice. It is clear that the ensemble of cost functions used to define the IES solution does not represent an exact sampling of the posterior-Bayes' probability density function. Also, the use of an ensemble representation for the gradient in IES introduces an additional approximation compared to using an exact analytic gradient. For ES-MDA, the convergence, as a function of increasing number of uniform update steps, is studied for a huge ensemble size. We illustrate that ES-MDA converges to a solution that differs from the Bayesian posterior. The convergence is also examined using a realistic sample size to study the impact of the number of realizations relative to the number of update steps. We have run multiple ES-MDA experiments to examine the impact of using different schemes for choosing the lengths of the update steps, and we have tried to understand which properties of the inverse problem imply that a non-uniform update step length is beneficial. Finally, we have examined the smoother methods with a highly nonlinear model to examine their properties and limitations in more extreme situations.
引用
收藏
页码:885 / 908
页数:24
相关论文
共 29 条
[1]   The Ensemble Kalman Filter in Reservoir Engineering-a Review [J].
Aanonsen, Sigurd I. ;
Naevdal, Geir ;
Oliver, Dean S. ;
Reynolds, Albert C. ;
Valles, Brice .
SPE JOURNAL, 2009, 14 (03) :393-412
[2]   An iterative ensemble Kalman smoother [J].
Bocquet, M. ;
Sakov, P. .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2014, 140 (682) :1521-1535
[3]  
Burgers G, 1998, MON WEATHER REV, V126, P1719, DOI 10.1175/1520-0493(1998)126<1719:ASITEK>2.0.CO
[4]  
2
[5]   Levenberg-Marquardt forms of the iterative ensemble smoother for efficient history matching and uncertainty quantification [J].
Chen, Yan ;
Oliver, Dean S. .
COMPUTATIONAL GEOSCIENCES, 2013, 17 (04) :689-703
[6]   Ensemble Randomized Maximum Likelihood Method as an Iterative Ensemble Smoother [J].
Chen, Yan ;
Oliver, Dean S. .
MATHEMATICAL GEOSCIENCES, 2012, 44 (01) :1-26
[7]   Analysis of the performance of ensemble-based assimilation of production and seismic data [J].
Emerick, Alexandre A. .
JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING, 2016, 139 :219-239
[8]   Ensemble smoother with multiple data assimilation [J].
Emerick, Alexandre A. ;
Reynolds, Albert C. .
COMPUTERS & GEOSCIENCES, 2013, 55 :3-15
[9]   History matching time-lapse seismic data using the ensemble Kalman filter with multiple data assimilations [J].
Emerick, Alexandre A. ;
Reynolds, Albert C. .
COMPUTATIONAL GEOSCIENCES, 2012, 16 (03) :639-659
[10]  
Evensen G, 2000, MON WEATHER REV, V128, P1852, DOI 10.1175/1520-0493(2000)128<1852:AEKSFN>2.0.CO