Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/100757
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dc.contributorDepartment of Land Surveying and Geo-Informaticsen_US
dc.creatorWang, Sen_US
dc.creatorHuang, GHen_US
dc.creatorBaetz, BWen_US
dc.creatorCai, XMen_US
dc.creatorAncell, BCen_US
dc.creatorFan, YRen_US
dc.date.accessioned2023-08-11T03:13:15Z-
dc.date.available2023-08-11T03:13:15Z-
dc.identifier.issn0022-1694en_US
dc.identifier.urihttp://hdl.handle.net/10397/100757-
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.rights© 2017 Elsevier B.V. All rights reserved.en_US
dc.rights© 2017. This manuscript version is made available under the CC-BY-NC-ND 4.0 license https://creativecommons.org/licenses/by-nc-nd/4.0/en_US
dc.rightsThe following publication Wang, S., Huang, G. H., Baetz, B. W., Cai, X. M., Ancell, B. C., & Fan, Y. R. (2017). Examining dynamic interactions among experimental factors influencing hydrologic data assimilation with the ensemble Kalman filter. Journal of Hydrology, 554, 743-757 is available at https://doi.org/10.1016/j.jhydrol.2017.09.052.en_US
dc.subjectData assimilationen_US
dc.subjectEnsemble Kalman filteren_US
dc.subjectHydrologic ensemble predictionen_US
dc.subjectInteractionen_US
dc.subjectStreamflowen_US
dc.subjectUncertaintyen_US
dc.titleExamining dynamic interactions among experimental factors influencing hydrologic data assimilation with the ensemble Kalman filteren_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage743en_US
dc.identifier.epage757en_US
dc.identifier.volume554en_US
dc.identifier.doi10.1016/j.jhydrol.2017.09.052en_US
dcterms.abstractThe ensemble Kalman filter (EnKF) is recognized as a powerful data assimilation technique that generates an ensemble of model variables through stochastic perturbations of forcing data and observations. However, relatively little guidance exists with regard to the proper specification of the magnitude of the perturbation and the ensemble size, posing a significant challenge in optimally implementing the EnKF. This paper presents a robust data assimilation system (RDAS), in which a multi-factorial design of the EnKF experiments is first proposed for hydrologic ensemble predictions. A multi-way analysis of variance is then used to examine potential interactions among factors affecting the EnKF experiments, achieving optimality of the RDAS with maximized performance of hydrologic predictions. The RDAS is applied to the Xiangxi River watershed which is the most representative watershed in China's Three Gorges Reservoir region to demonstrate its validity and applicability. Results reveal that the pairwise interaction between perturbed precipitation and streamflow observations has the most significant impact on the performance of the EnKF system, and their interactions vary dynamically across different settings of the ensemble size and the evapotranspiration perturbation. In addition, the interactions among experimental factors vary greatly in magnitude and direction depending on different statistical metrics for model evaluation including the Nash–Sutcliffe efficiency and the Box–Cox transformed root-mean-square error. It is thus necessary to test various evaluation metrics in order to enhance the robustness of hydrologic prediction systems.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of hydrology, Nov. 2017, v. 554, p. 743-757en_US
dcterms.isPartOfJournal of hydrologyen_US
dcterms.issued2017-11-
dc.identifier.scopus2-s2.0-85030700221-
dc.description.validate202305 bckwen_US
dc.description.oaAccepted Manuscripten_US
dc.identifier.FolderNumberLSGI-0345-
dc.description.fundingSourceOthersen_US
dc.description.fundingTextHong Kong Polytechnic Universityen_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS6786933-
dc.description.oaCategoryGreen (AAM)en_US
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