The use of GRACE data to monitor natural and anthropogenic induced variations in water availability across Africa

被引:137
作者
Ahmed, Mohamed [1 ,2 ]
Sultan, Mohamed [1 ]
Wahr, John [3 ]
Yan, Eugene [4 ]
机构
[1] Western Michigan Univ, Dept Geosci, Kalamazoo, MI 49008 USA
[2] Suez Canal Univ, Fac Sci, Dept Geol, Ismailia 41522, Egypt
[3] Univ Colorado, Dept Phys, Boulder, CO 80309 USA
[4] Argonne Natl Lab, Div Environm Sci, Argonne, IL 60439 USA
基金
美国国家航空航天局;
关键词
GRACE; TWS; Africa; Water availability; Climate change; Anthropogenic effects; NORTH-ATLANTIC OSCILLATION; DROUGHT SEVERITY INDEX; CLIMATE EXPERIMENT; GRAVITY RECOVERY; GROUNDWATER DEPLETION; SATELLITE GRAVITY; GLOBAL PRECIPITATION; SST MODES; RAINFALL; STORAGE;
D O I
10.1016/j.earscirev.2014.05.009
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Inter-annual trends in terrestrial water storage (TWS) were extracted from monthly (01/2003-09/2012) Gravity Recovery and Climate Experiment (GRACE) data acquired over Africa and correlated (in a geographic information system [GIS] environment) with relevant temporal remote sensing, geologic, and hydrologic datasets. Findings include the following: (1) large sectors of Africa are undergoing statistically significant TWS variations (+44 mm/yr to -15 mm/yr) due to natural and anthropogenic causes; (2) warming of the tropical Atlantic Ocean apparently intensified Atlantic monsoons and increased precipitation and TWS over western and central Africa; (3) warming in the central Indian Ocean decreased precipitation and TWS over eastern Africa; (4) the high frequency of flooding events increased TWS over the Zambezi and Okavango basins; (5) extraction of fossil groundwater decreased TWS over the Saharan aquifers; (6) deforestation decreased TWS in three subbasins (Ubangi, Congo, and Sangha) of the Congo River Basin; and (7) the construction of dams increased TWS in the Blue Nile and Atbara subbasins. Given the 10 years of monthly GRACE data acquired on the subbasin scale across the globe, as well as the plans underway for deployment of a GRACE-FO and GRACE-II, using GRACE-derived TWS data should be considered an alternative, viable index for measuring temporal and spatial variations in water availability. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:289 / 300
页数:12
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