Conditioning Multi-Gaussian Groundwater Flow Parameters to Transient Hydraulic Head and Flowrate Data With Iterative Ensemble Smoothers: A Synthetic Case Study

Over the last decade, data assimilation methods based on the ensemble Kalman filter (EnKF) have been particularly explored in various geoscience fields to solve inverse problems. Although this type of ensemble methods can handle high-dimensional systems, they assume that the errors coming from wheth...

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Main Authors: Dan-Thuy Lam, Jaouher Kerrou, Philippe Renard, Hakim Benabderrahmane, Pierre Perrochet
Format: Article
Language:English
Published: Frontiers Media S.A. 2020-06-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/feart.2020.00202/full
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spelling doaj-3ae9a6d348bb438c9d58a8b5222c817f2020-11-25T02:27:26ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632020-06-01810.3389/feart.2020.00202532270Conditioning Multi-Gaussian Groundwater Flow Parameters to Transient Hydraulic Head and Flowrate Data With Iterative Ensemble Smoothers: A Synthetic Case StudyDan-Thuy Lam0Jaouher Kerrou1Philippe Renard2Hakim Benabderrahmane3Pierre Perrochet4Centre for Hydrogeology and Geothermics (CHYN), University of Neuchâtel, Neuchâtel, SwitzerlandCentre for Hydrogeology and Geothermics (CHYN), University of Neuchâtel, Neuchâtel, SwitzerlandCentre for Hydrogeology and Geothermics (CHYN), University of Neuchâtel, Neuchâtel, SwitzerlandFrench National Radioactive Waste Management Agency (ANDRA), Châtenay-Malabry, FranceCentre for Hydrogeology and Geothermics (CHYN), University of Neuchâtel, Neuchâtel, SwitzerlandOver the last decade, data assimilation methods based on the ensemble Kalman filter (EnKF) have been particularly explored in various geoscience fields to solve inverse problems. Although this type of ensemble methods can handle high-dimensional systems, they assume that the errors coming from whether the observations or the numerical model are multivariate Gaussian. To handle existing non-linearities between the observations and the variables to estimate, iterative methods have been proposed. In this paper, we investigate the feasibility of using the ensemble smoother and two iterative variants for the calibration of a synthetic 2D groundwater model inspired by a real nuclear storage problem in France. Using the same set of sparse and transient flow data, we compare the results of each method when employing them to condition an ensemble of multi-Gaussian groundwater flow parameter fields. In particular, we explore the benefit of transforming the state observations to improve the parameter identification performed by one of the two iterative algorithms tested. Despite the favorable case of a multi-Gaussian parameter distribution addressed, we show the importance of defining an ensemble size of at least 200 to obtain sufficiently accurate parameter and uncertainty estimates for the groundwater flow inverse problem considered.https://www.frontiersin.org/article/10.3389/feart.2020.00202/fullinverse problemtransient groundwater flowparameter identificationiterative ensemble smootherdata assimilationuncertainty
collection DOAJ
language English
format Article
sources DOAJ
author Dan-Thuy Lam
Jaouher Kerrou
Philippe Renard
Hakim Benabderrahmane
Pierre Perrochet
spellingShingle Dan-Thuy Lam
Jaouher Kerrou
Philippe Renard
Hakim Benabderrahmane
Pierre Perrochet
Conditioning Multi-Gaussian Groundwater Flow Parameters to Transient Hydraulic Head and Flowrate Data With Iterative Ensemble Smoothers: A Synthetic Case Study
Frontiers in Earth Science
inverse problem
transient groundwater flow
parameter identification
iterative ensemble smoother
data assimilation
uncertainty
author_facet Dan-Thuy Lam
Jaouher Kerrou
Philippe Renard
Hakim Benabderrahmane
Pierre Perrochet
author_sort Dan-Thuy Lam
title Conditioning Multi-Gaussian Groundwater Flow Parameters to Transient Hydraulic Head and Flowrate Data With Iterative Ensemble Smoothers: A Synthetic Case Study
title_short Conditioning Multi-Gaussian Groundwater Flow Parameters to Transient Hydraulic Head and Flowrate Data With Iterative Ensemble Smoothers: A Synthetic Case Study
title_full Conditioning Multi-Gaussian Groundwater Flow Parameters to Transient Hydraulic Head and Flowrate Data With Iterative Ensemble Smoothers: A Synthetic Case Study
title_fullStr Conditioning Multi-Gaussian Groundwater Flow Parameters to Transient Hydraulic Head and Flowrate Data With Iterative Ensemble Smoothers: A Synthetic Case Study
title_full_unstemmed Conditioning Multi-Gaussian Groundwater Flow Parameters to Transient Hydraulic Head and Flowrate Data With Iterative Ensemble Smoothers: A Synthetic Case Study
title_sort conditioning multi-gaussian groundwater flow parameters to transient hydraulic head and flowrate data with iterative ensemble smoothers: a synthetic case study
publisher Frontiers Media S.A.
series Frontiers in Earth Science
issn 2296-6463
publishDate 2020-06-01
description Over the last decade, data assimilation methods based on the ensemble Kalman filter (EnKF) have been particularly explored in various geoscience fields to solve inverse problems. Although this type of ensemble methods can handle high-dimensional systems, they assume that the errors coming from whether the observations or the numerical model are multivariate Gaussian. To handle existing non-linearities between the observations and the variables to estimate, iterative methods have been proposed. In this paper, we investigate the feasibility of using the ensemble smoother and two iterative variants for the calibration of a synthetic 2D groundwater model inspired by a real nuclear storage problem in France. Using the same set of sparse and transient flow data, we compare the results of each method when employing them to condition an ensemble of multi-Gaussian groundwater flow parameter fields. In particular, we explore the benefit of transforming the state observations to improve the parameter identification performed by one of the two iterative algorithms tested. Despite the favorable case of a multi-Gaussian parameter distribution addressed, we show the importance of defining an ensemble size of at least 200 to obtain sufficiently accurate parameter and uncertainty estimates for the groundwater flow inverse problem considered.
topic inverse problem
transient groundwater flow
parameter identification
iterative ensemble smoother
data assimilation
uncertainty
url https://www.frontiersin.org/article/10.3389/feart.2020.00202/full
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