Data assimilation with multiple types of observation boreholes via the ensemble Kalman filter embedded within stochastic moment equations
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Department of Hydrology and Atmospheric Sciences, University of ArizonaIssue Date
2021
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Copernicus GmbHCitation
Xia, C. A., Luo, X., Hu, B. X., Riva, M., & Guadagnini, A. (2021). Data assimilation with multiple types of observation boreholes via the ensemble Kalman filter embedded within stochastic moment equations. Hydrology and Earth System Sciences, 25(4), 1689-1709.Rights
Copyright © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
We employ an approach based on the ensem ble Kalman filter coupled with stochastic moment equa tions (MEs-EnKF) of groundwater flow to explore the de pendence of conductivity estimates on the type of available information about hydraulic heads in a three-dimensional randomly heterogeneous field where convergent flow driven by a pumping well takes place. To this end, we consider three types of observation devices corresponding to (i) multi node monitoring wells equipped with packers (Type A) and (ii) partially (Type B) and (iii) fully (Type C) screened wells. We ground our analysis on a variety of synthetic test cases associated with various configurations of these observation wells. Moment equations are approximated at second order (in terms of the standard deviation of the natural logarithm, Y , of conductivity) and are solved by an efficient transient numerical scheme proposed in this study. The use of an infla tion factor imposed to the observation error covariance ma trix is also analyzed to assess the extent at which this can strengthen the ability of the MEs-EnKF to yield appropri ate conductivity estimates in the presence of a simplified modeling strategy where flux exchanges between monitor ing wells and aquifer are neglected. Our results show that (i) the configuration associated with Type A monitoring wells leads to conductivity estimates with the (overall) best qual ity, (ii) conductivity estimates anchored on information from Type B and C wells are of similar quality, (iii) inflation of the measurement-error covariance matrix can improve conduc tivity estimates when a simplified flow model is adopted, and (iv) when compared with the standard Monte Carlo-based EnKF method, the MEs-EnKF can efficiently and accurately estimate conductivity and head fields. © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License.Note
Open access journalISSN
1027-5606Version
Final published versionae974a485f413a2113503eed53cd6c53
10.5194/hess-25-1689-2021
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Except where otherwise noted, this item's license is described as Copyright © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License.