Multi-source satellite reveals the heterogeneity in water storage change over northwestern China in recent decades

被引:6
|
作者
Liu, Qing [1 ,2 ]
Xu, Yuyue [1 ,2 ,3 ]
Chen, Jianli [4 ,5 ]
Cheng, Xing [1 ,2 ]
机构
[1] Nanjing Univ, Sch Geog & Ocean Sci, Nanjing 210023, Jiangsu, Peoples R China
[2] Nanjing Univ, Jiangsu Prov Key Lab Geog Informat Sci & Technol, Nanjing 210023, Peoples R China
[3] Nanjing Univ, Frontiers Sci Ctr Crit Earth Mat Cycling, Nanjing 210023, Peoples R China
[4] Hong Kong Polytech Univ, Dept Land Surveying & Geoinformat, Hung Hom, Kowloong, Hong Kong, Peoples R China
[5] Hong Kong Polytech Univ, Res Inst Land & Space, Hung Hom, Kowloong, Hong Kong, Peoples R China
基金
中国国家自然科学基金;
关键词
Water storage change; Northwestern China; GRACE; Climatic factors; Human activities; GLOBAL HYDROLOGICAL MODEL; TARIM RIVER-BASIN; TIBETAN PLATEAU; CLIMATE-CHANGE; GRACE DATA; DATA ASSIMILATION; GROUNDWATER; XINJIANG; LAKES; RESOURCES;
D O I
10.1016/j.jhydrol.2023.129953
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The northwestern China (NWC) generally suffers from severe water shortages. To improve the management and utilization of the limited water storage in NWC, it is crucial to explore the distribution and variation of water storage. Here, we obtained the variations of terrestrial water storage (TWS), surface water area (SWA), and groundwater storage (GWS) in NWC (which refers to Xinjiang Uyghur Autonomous Region in the study) from 2002 to 2018 based on multi-source satellite data, and analyzed the factors influencing water storage changes. The results indicated that (1) SWA exhibited an increasing trend with 40.90 km2/year from 2002 to 2018 based on main lakes/reservoirs and rivers water area in NWC, due to the increase of precipitation and glacier melting. TWS and GWS showed a decreasing trend with a mean rate of -1.25 mm/year and -1.08 mm/year from 2002 to 2018 in NWC, respectively, due to the increase of arable land area and water consumption. (2) SWA in northern and southern NWC showed a decrease (-0.72 km2/year) and an increase (51.14 km2/year) from 2002 to 2018, respectively. The different rates are due to regional precipitation and temperature variations. TWS in northern and southern NWC showed a declining of -0.14 mm/year and -1.94 mm/year, respectively. GWS in northern and southern NWC showed a declining of -0.55 mm/year and -1.72 mm/year, respectively. The differences are related to the greater evapotranspiration and irrigation water consumption in southern than northern NWC. This study enriches the information on water storage in NWC and provides useful guidance for local water resource management and protection.
引用
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页数:15
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