Continuing Severe Water Shortage in the Water‐Receiving Area of the South‐To‐North Water Diversion Eastern Route Project From 2002 to 2020

Author:

Xu Yuyue123ORCID,Gun Zhao12ORCID,Zhao Jianwei12,Chen Jianli4ORCID,Liu Qing12,Cheng Xing12ORCID,Sutanudjaja Edwin H.5,Wang Jida6ORCID,Liu Hehua7,Zhan Wenfeng8ORCID

Affiliation:

1. School of Geography and Ocean Science Nanjing University Nanjing China

2. Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology Nanjing University Nanjing China

3. Frontiers Science Center for Critical Earth Material Cycling Nanjing University Nanjing China

4. Department of Land Surveying and Geo‐Informatics and Research Institute for Land and Space The Hong Kong Polytechnic University Kowloong China

5. Faculty of Geosciences Department of Physical Geography Utrecht University Utrecht The Netherlands

6. Department of Geography and Geographic Information Science University of Illinois Urbana–Champaign Urbana IL USA

7. East China Mineral Exploration and Development Bureau Nanjing China

8. International Institute of Earth System Science Nanjing University Nanjing China

Abstract

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.

Funder

National Key Research and Development Program of China

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

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