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dc.date.accessioned2024-03-15T17:46:32Z
dc.date.available2024-03-15T17:46:32Z
dc.date.created2023-12-02T16:45:26Z
dc.date.issued2023
dc.identifier.citationSheng, Sheng Chen, Hua Lin, Kangling Zhou, Yanlai Wang, Jinxing Chen, Jie Xiong, Lihua Guo, Shenglian Xu, Chong-Yu . Enhancing runoff simulation precision in the critical zone through spatiotemporal interpolation of areal rainfall with matrix decomposition. Hydrological Processes. 2023, 37(11)
dc.identifier.urihttp://hdl.handle.net/10852/109621
dc.description.abstractAbstract Modelling hydrological process in the critical zone not only contributes to a better understanding of interactions across different Earth surface spheres but also holds significant practical implications for water resource management and disaster prevention. Rainfall‐runoff simulation in critical zones is particularly challenging due to the amalgamation of temporal and spatial complexity, rainfall variability, and data limitations. As a pivotal input variable of hydrological models, accurate estimation of areal rainfall is critical to successful runoff simulation. However, most estimation methods ignore temporal information, thereby increasing uncertainty in rainfall estimation and constraining the precision of rainfall‐runoff simulation. In this study, the matrix decomposition‐based estimation method (F‐SVD), which considers the spatial and temporal correlation of the rainfall process is employed to estimate areal rainfall. The superiority of the method in producing two‐dimensional rainfall information is evaluated through its application in runoff simulation with the Xin'anjiang model. The simulation results of selected flood events in the Jianxi basin in southeast China, spanning from 2009 to 2019, are compared with those of two widely used rainfall estimation methods, namely Arithmetical Mean (AM) and Thiessen Polygons (TP). The results show that (1) F‐SVD not only produces the highest Pearson correlation coefficient between rainfall and runoff series but also reduces the number of flood events with abnormal rainfall‐runoff relationships; (2) the Xin'anjiang model based on F‐SVD achieves the highest Nash‐Sutcliffe efficiency and lowest Relative Error, and performs best in simulating peak flow and its occurrence time as compared to AM and TP. This study contributes to a finer characterization of watershed rainfall distribution, enhancing the accuracy and sharpness of runoff simulation. It provides reliable data support for critical zone research and offers a scientific foundation for rationally allocating and managing water resources.
dc.languageEN
dc.publisherWiley-Interscience Publishers
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleEnhancing runoff simulation precision in the critical zone through spatiotemporal interpolation of areal rainfall with matrix decomposition
dc.title.alternativeENEngelskEnglishEnhancing runoff simulation precision in the critical zone through spatiotemporal interpolation of areal rainfall with matrix decomposition
dc.typeJournal article
dc.creator.authorSheng, Sheng
dc.creator.authorChen, Hua
dc.creator.authorLin, Kangling
dc.creator.authorZhou, Yanlai
dc.creator.authorWang, Jinxing
dc.creator.authorChen, Jie
dc.creator.authorXiong, Lihua
dc.creator.authorGuo, Shenglian
dc.creator.authorXu, Chong-Yu
cristin.unitcode185,15,22,60
cristin.unitnameSeksjon for naturgeografi og hydrologi
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode1
dc.identifier.cristin2207789
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Hydrological Processes&rft.volume=37&rft.spage=&rft.date=2023
dc.identifier.jtitleHydrological Processes
dc.identifier.volume37
dc.identifier.issue11
dc.identifier.pagecount0
dc.identifier.doihttps://doi.org/10.1002/hyp.15039
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn0885-6087
dc.type.versionAcceptedVersion
cristin.articleide202301052
dc.relation.projectNFR/274310


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