Increased water storage in North America and Scandinavia from GRACE gravity data

被引:0
|
作者
Wang, Hansheng [1 ]
Jia, Lulu [1 ,2 ,4 ]
Steffen, Holger [3 ,6 ]
Wu, Patrick [3 ]
Jiang, Liming [1 ]
Hsu, Houtse [1 ]
Xiang, Longwei [1 ,2 ]
Wang, Zhiyong [5 ]
Hu, Bo [1 ,2 ]
机构
[1] Chinese Acad Sci, Inst Geodesy & Geophys, State Key Lab Geodesy & Earths Dynam, Wuhan 430077, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Univ Calgary, Dept Geosci, Calgary, AB T2N 1N4, Canada
[4] Natl Earthquake Infrastruct Serv, Beijing 100036, Peoples R China
[5] Shandong Univ Technol, Dept Surveying Engn, Zibo 255049, Peoples R China
[6] Lantmateriet, S-80182 Gavle, Sweden
基金
美国国家科学基金会; 加拿大自然科学与工程研究理事会; 中国国家自然科学基金;
关键词
GLACIAL ISOSTATIC-ADJUSTMENT; MANTLE VISCOSITY; ICE-5G VM2; MODEL;
D O I
10.1038/NGEO1652
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Space-borne gravity data from the Gravity Recovery and Climate Experiment (GRACE) have revealed trends in present-day continental water storage in many parts of the world. In North America and northern Europe, it has been difficult to provide reliable estimates because of the strong background signals of glacial isostatic adjustment(1). Attempts to separate the hydrologic signal from the background with numerical models(2) are affected by uncertainties in our understanding of the precise glacial history and mantle viscosity(3,4). Here we use a combination of GRACE data and measurements from the global positioning system to separate the hydrological signals without any model assumptions. According to our estimates, water storage in central North America increased by 43.0 +/- 5.0 Gt yr(-1) over the past decade. We attribute this increase to a recovery in terrestrial water storage after the extreme Canadian Prairies drought between 1999 and 2005. We find a smaller rise in water storage in southern Scandinavia, by 2.3 +/- 0.8 Gt yr(-1). In both North America and Scandinavia, our computed increases in water storage are consistent with long-term observations of terrestrial water level. We suggest that the detected mass gains in terrestrial water storage need to be taken into account in studies on global sea-level rise.
引用
收藏
页码:38 / 42
页数:5
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