Monitoring small reservoirs' storage with satellite remote sensing in inaccessible areas

被引:85
作者
Avisse, Nicolas [1 ]
Tilmant, Amaury [1 ]
Muller, Marc Francois [2 ]
Zhang, Hua [3 ]
机构
[1] Univ Laval, Dept Civil Engn & Water Engn, Quebec City, PQ G1V 0A6, Canada
[2] Univ Notre Dame, Dept Civil & Environm Engn & Earth Sci, Notre Dame, IN 46556 USA
[3] Texas A&M Univ, Sch Engn & Comp Sci, Dept Engn, Corpus Christi, TX 78412 USA
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;
关键词
DIFFERENCE WATER INDEX; UPPER EAST REGION; SEMIARID ENVIRONMENT; LEVEL CHANGES; CLOUD SHADOW; MODIS IMAGES; LAKE; ALTIMETRY; VOLUME; TOPEX/POSEIDON;
D O I
10.5194/hess-21-6445-2017
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In river basins with water storage facilities, the availability of regularly updated information on reservoir level and capacity is of paramount importance for the effective management of those systems. However, for the vast majority of reservoirs around the world, storage levels are either not measured or not readily available due to financial, political, or legal considerations. This paper proposes a novel approach using Landsat imagery and digital elevation models (DEMs) to retrieve information on storage variations in any inaccessible region. Unlike existing approaches, the method does not require any in situ measurement and is appropriate for monitoring small, and often undocumented, irrigation reservoirs. It consists of three recovery steps: (i) a 2-D dynamic classification of Landsat spectral band information to quantify the surface area of water, (ii) a statistical correction of DEM data to characterize the topography of each reservoir, and (iii) a 3-D reconstruction algorithm to correct for clouds and Landsat 7 Scan Line Corrector failure. The method is applied to quantify reservoir storage in the Yarmouk basin in southern Syria, where ground monitoring is impeded by the ongoing civil war. It is validated against available in situ measurements in neighbouring Jordanian reservoirs. Coefficients of determination range from 0.69 to 0.84, and the normalized root-mean-square error from 10 to 16% for storage estimations on six Jordanian reservoirs with maximal water surface areas ranging from 0.59 to 3.79 km(2).
引用
收藏
页码:6445 / 6459
页数:15
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