Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/113219
PIRA download icon_1.1View/Download Full Text
DC FieldValueLanguage
dc.contributorDepartment of Land Surveying and Geo-Informatics-
dc.contributorResearch Institute for Land and Space-
dc.creatorXu, Y-
dc.creatorGun, Z-
dc.creatorZhao, J-
dc.creatorChen, J-
dc.creatorLiu, Q-
dc.creatorCheng, X-
dc.creatorSutanudjaja, EH-
dc.creatorWang, J-
dc.creatorLiu, H-
dc.creatorZhan, W-
dc.date.accessioned2025-05-29T07:59:25Z-
dc.date.available2025-05-29T07:59:25Z-
dc.identifier.issn0043-1397-
dc.identifier.urihttp://hdl.handle.net/10397/113219-
dc.language.isoenen_US
dc.publisherWiley-Blackwell Publishing, Inc.en_US
dc.rights© 2023. American Geophysical Union. All Rights Reserved.en_US
dc.titleContinuing severe water shortage in the water-receiving area of the South-To-North Water Diversion Eastern Route Project from 2002 to 2020en_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume59-
dc.identifier.issue10-
dc.identifier.doi10.1029/2022WR034365-
dcterms.abstractThe water-receiving area of the South-to-North Water Diversion Eastern Route Project (SNWDP-ER) is one of the most severely affected water-shortage areas in China, and no previous study has been conducted on the changes in water storage in this area. In this study, we combined the latest Gravity Recovery and Climate Experiment (GRACE) And GRACE Follow-On products with global models for the first time to analyze changes in water storages in this area from 2002 to 2020, and to investigate the effects of climate change and human activity on changes in water storage. We found that SNWDP-ER aided the recovery of surface water (nongroundwater) with a recovery rate of 9.44 ± 1.65 mm/yr after its implementation, but had little effect on the recovery of groundwater and terrestrial water storage in the water-receiving area. Before the SNWDP-ER was implemented, the rates of decrease of groundwater and terrestrial water storage were only −1.59 ± 0.58 and −5.18 ± 0.75 mm/yr, respectively. After implementation, the rates of decrease of groundwater and terrestrial water storage were −17.7 ± 1.27 and −8.16 ± 1.18 mm/yr, respectively. Groundwater decline, accelerated by human activity and climate change, has led to an accelerated decline in terrestrial water storage. Effects of SNWDP-ER and stringent policies reducing groundwater use, along with largely increased precipitation in North China on groundwater storage after year 2020 need to be examined in the future. Our results have important implications for the management and evaluation of SNWDP-ER.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationWater resources research, Oct. 2023, v. 59, no. 10, e2022WR034365-
dcterms.isPartOfWater resources research-
dcterms.issued2023-10-
dc.identifier.scopus2-s2.0-85174447414-
dc.identifier.eissn1944-7973-
dc.identifier.artne2022WR034365-
dc.description.validate202505 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Othersen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextThe National Key Research and Development Program of China (2022YFF0711603); the Fundamental Research Funds for the Central Universities (0209-14380093, 0209-14380097); the Frontiers Science Center for Critical Earth Material Cycling Fund (JBGS2102); National Natural Science Foundation of China (no. 41671423); the Ministry Science and Technology Development of China-Data Sharing Infrastructure of Earth System Science (2005DKA32300)en_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryVoR alloweden_US
Appears in Collections:Journal/Magazine Article
Files in This Item:
File Description SizeFormat 
Xu_Continuing_Severe_Water.pdf6.96 MBAdobe PDFView/Open
Open Access Information
Status open access
File Version Version of Record
Access
View full-text via PolyU eLinks SFX Query
Show simple item record

Google ScholarTM

Check

Altmetric


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.