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dc.date.accessioned2019-12-06T19:02:15Z
dc.date.available2019-12-06T19:02:15Z
dc.date.created2019-01-14T21:35:15Z
dc.date.issued2018
dc.identifier.citationWang, Hui-Min Chen, Jie Cannon, Alex J. Xu, Chong-Yu Chen, Hua . Transferability of climate simulation uncertainty to hydrological impacts. Hydrology and Earth System Sciences. 2018, 22(7), 3739-3759
dc.identifier.urihttp://hdl.handle.net/10852/71265
dc.description.abstractConsidering rapid increases in the number of climate model simulations being produced by modelling centres, it is often infeasible to use all of them in climate change impact studies. In order to thoughtfully select subsets of climate simulations from a large ensemble, several envelope-based methods have been proposed. The subsets are expected to cover a similar uncertainty envelope to the full ensemble in terms of climate variables. However, it is not a given that the uncertainty in hydrological impacts will be similarly well represented. Therefore, this study investigates the transferability of climate uncertainty related to the choice of climate simulations to hydrological impacts. Two envelope-based selection methods, K means clustering and the Katsavounidis–Kuo–Zhang (KKZ) method, are used to select subsets from an ensemble of 50 climate simulations over two watersheds with very different climates using 31 precipitation and temperature variables. Transferability is evaluated by comparing uncertainty coverage between climate variables and 17 hydrological variables simulated by a hydrological model. The importance of choosing climate variables properly when selecting subsets is investigated by including and excluding temperature variables. Results show that KKZ performs better than K means at selecting subsets of climate simulations for hydrological impacts, and the uncertainty coverage of climate variables is similar to that of hydrological variables. The subset of the first 10 simulations covers over 85 % of total uncertainty. As expected, temperature variables are important for the snow-related watershed, but less important for the rainfall-driven watershed. Overall, envelope-based selection of around 10 climate simulations, based on climate variables that characterize the physical processes controlling the hydrology of the watershed, is recommended for hydrological impact studies.
dc.languageEN
dc.publisherCopernicus
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleTransferability of climate simulation uncertainty to hydrological impacts
dc.typeJournal article
dc.creator.authorWang, Hui-Min
dc.creator.authorChen, Jie
dc.creator.authorCannon, Alex J.
dc.creator.authorXu, Chong-Yu
dc.creator.authorChen, Hua
cristin.unitcode185,15,22,60
cristin.unitnameSeksjon for naturgeografi og hydrologi
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.cristin1656737
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 and Earth System Sciences&rft.volume=22&rft.spage=3739&rft.date=2018
dc.identifier.jtitleHydrology and Earth System Sciences
dc.identifier.volume22
dc.identifier.issue7
dc.identifier.startpage3739
dc.identifier.endpage3759
dc.identifier.doihttps://doi.org/10.5194/hess-22-3739-2018
dc.identifier.urnURN:NBN:no-74400
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn1027-5606
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/71265/2/hess-22-3739-2018.pdf
dc.type.versionPublishedVersion


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