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dc.date.accessioned2024-04-03T16:27:53Z
dc.date.available2024-04-03T16:27:53Z
dc.date.created2023-10-13T07:50:37Z
dc.date.issued2023
dc.identifier.citationJiang, Shanhu Zhu, Yongwei Ren, Liliang Yan, Denghua Liu, Ying Cui, Hao Wang, Menghao Xu, Chong-Yu . A Complementary Streamflow Attribution Framework Coupled Climate, Vegetation and Water Withdrawal. Water resources management. 2023, 37, 4807-4822
dc.identifier.urihttp://hdl.handle.net/10852/110316
dc.description.abstractQuantifying the contributions of climate change (CC) and human activities (HA) to streamflow alteration is significant for effective water resources management. However, numerous studies fail to differentiate the individual impacts of various HA on streamflow. In this study, a comprehensive streamflow attribution framework that incorporates climate, vegetation, and water withdrawal (WW) was proposed. In this framework, traditional streamflow attribution methods such as statistical analysis (Double Mass Curve and Slope Change Ratio of Accumulative Quantity), elasticity (Budyko), and modeling simulation (Variable Infiltration Capacity and Long Short-term Memory) are employed to separate the influence of meteorological factors (MF) on streamflow. Subsequently, the impacts of WW on streamflow are assessed using global WW data. The Residual Analysis method is utilized to quantify the effects of vegetation alteration caused by both CC (Lcc) and HA (Lha) on streamflow alteration. To demonstrate the applicability of our proposed framework, two stations, Xianyang and Huaxian, located within the Weihe River Basin in Northwest China were selected as the case study area. The results demonstrated that compared to the baseline period (1961–1990), the average contributions of MF, Lcc, Lha, and WW to streamflow reduction during the variation periods (1991–2019) were as follows: for the Xianyang station, 26.0%, 13.5%, 30.9%, and 29.6% respectively; and for the Huaxian station, 28.9%, 5.5%, 17.7%, and 47.9% respectively. Additionally, during the variation periods, the contributions of CC and HA to vegetation variation were 30.5% and 69.5% respectively in Xianyang, and 23.7% and 76.3% respectively in Huaxian. The framework developed herein also provides a solution for quantifying the indirect effects of CC on streamflow through vegetation.
dc.languageEN
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleA Complementary Streamflow Attribution Framework Coupled Climate, Vegetation and Water Withdrawal
dc.title.alternativeENEngelskEnglishA Complementary Streamflow Attribution Framework Coupled Climate, Vegetation and Water Withdrawal
dc.typeJournal article
dc.creator.authorJiang, Shanhu
dc.creator.authorZhu, Yongwei
dc.creator.authorRen, Liliang
dc.creator.authorYan, Denghua
dc.creator.authorLiu, Ying
dc.creator.authorCui, Hao
dc.creator.authorWang, Menghao
dc.creator.authorXu, Chong-Yu
cristin.unitcode185,15,22,0
cristin.unitnameInstitutt for geofag
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode1
dc.identifier.cristin2184295
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Water resources management&rft.volume=37&rft.spage=4807&rft.date=2023
dc.identifier.jtitleWater resources management
dc.identifier.volume37
dc.identifier.issue12
dc.identifier.startpage4807
dc.identifier.endpage4822
dc.identifier.doihttps://doi.org/10.1007/s11269-023-03582-1
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn0920-4741
dc.type.versionAcceptedVersion


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