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dc.date.accessioned2020-03-04T19:26:00Z
dc.date.available2020-03-04T19:26:00Z
dc.date.created2018-11-29T12:33:07Z
dc.date.issued2018
dc.identifier.citationJiang, Shanhu Ren, Liliang Xu, Chong-Yu Liu, Shuya Yuan, Fei Yang, Xiaoli . Quantifying multi-source uncertainties in multi-model predictions using the Bayesian model averaging scheme. Hydrology Research. 2018, 49(3), 954-970
dc.identifier.urihttp://hdl.handle.net/10852/73684
dc.description.abstractThis study focuses on a quantitative multi-source uncertainty analysis of multi-model predictions. Three widely used hydrological models, i.e., Xinanjiang (XAJ), hybrid rainfall–runoff (HYB), and HYMOD (HYM), were calibrated by two parameter optimization algorithms, namely, shuffled complex evolution (SCE-UA) method and shuffled complex evolution metropolis (SCEM-UA) method on the Mishui basin, south China. The input uncertainty was quantified by utilizing a normally distributed error multiplier. The ensemble simulation sets calculated from the three models were combined using the Bayesian model averaging (BMA) method. Results indicate the following. (1) Both SCE-UA and SCEM-UA resulted in good and comparable streamflow simulations. Specifically, the SCEM-UA implied parameter uncertainty and provided the posterior distribution of the parameters. (2) In terms of the precipitation input uncertainty, precision of streamflow simulations did not improve remarkably. (3) The BMA combination not only improved the precision of streamflow prediction, but also quantified the uncertainty bounds of the simulation. (4) The prediction interval calculated using the SCEM-UA-based BMA combination approach appears superior to that calculated using the SCE-UA-based BMA combination for both high flows and low flows. Results suggest that the comprehensive uncertainty analysis by using the SCEM-UA algorithm and BMA method is superior for streamflow predictions and flood forecasting.
dc.languageEN
dc.titleQuantifying multi-source uncertainties in multi-model predictions using the Bayesian model averaging scheme
dc.typeJournal article
dc.creator.authorJiang, Shanhu
dc.creator.authorRen, Liliang
dc.creator.authorXu, Chong-Yu
dc.creator.authorLiu, Shuya
dc.creator.authorYuan, Fei
dc.creator.authorYang, Xiaoli
cristin.unitcode185,15,22,0
cristin.unitnameInstitutt for geofag
cristin.ispublishedtrue
cristin.fulltextpreprint
cristin.qualitycode1
dc.identifier.cristin1636906
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Hydrology Research&rft.volume=49&rft.spage=954&rft.date=2018
dc.identifier.jtitleHydrology Research
dc.identifier.volume49
dc.identifier.issue3
dc.identifier.startpage954
dc.identifier.endpage970
dc.identifier.doihttps://doi.org/10.2166/nh.2017.272
dc.identifier.urnURN:NBN:no-76804
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn1998-9563
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/73684/1/Jiang%2BShanhu%2BHydrology-D-16-00272_R1.pdf
dc.type.versionAcceptedVersion


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