MODIS observations of the bottom topography and its inter-annual variability of Poyang Lake

被引:112
作者
Feng, Lian [1 ,2 ]
Hu, Chuanmin [2 ]
Chen, Xiaoling [1 ,3 ]
Li, Rongfang [4 ,5 ]
Tian, Liqiao [1 ]
Murch, Brock [2 ]
机构
[1] Wuhan Univ, State Key Lab Informat Engn Surveying Mapping & R, Wuhan 430079, Peoples R China
[2] Univ S Florida, Coll Marine Sci, St Petersburg, FL 33701 USA
[3] JiangXi Normal Univ, Minist Educ, Key Lab Poyang Lake Wetland & Watershed Res, Nanchang 330022, Peoples R China
[4] Donghua Univ, Coll Informat Sci & Technol, Shanghai 201620, Peoples R China
[5] Jiangxi Prov Inst Water Sci, Nanchang 330029, Peoples R China
基金
中国国家自然科学基金;
关键词
Poyang Lake; Bottom topography; Bathymetry; MODIS; Inundation; Remote sensing; SHALLOW-WATER BATHYMETRY; FLOOD FREQUENCY; DYNAMICS; DEPTHS; LIDAR; INLET; RIVER;
D O I
10.1016/j.rse.2011.06.013
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Using MODIS 250-m resolution data, we developed a novel approach to derive the bottom topography of Poyang Lake, the largest freshwater lake of China (>3000 km(2) at maximum inundation) for every year between 2000 and 2009. The approach differs from other traditional methods (sonar, Lidar, optical inversion, and Radar) but takes advantage of the fast-changing nature of the lake's inundation area. On every image, the water/land boundary is effectively a topographic isobath after correction for the water level gradient. Thus, the -10/year carefully selected MODIS images provided incremental topographic isobaths, from which bottom topography was derived every year. Such-derived topographic maps were validated using limited historical data and other consistency checks. Most of the lake bottom showed an elevation of 12 m to 17 m (referenced against the elevation reference of the Woosung Horizontal Zero). Significant inter-annual variability of the bottom topography from 2000 to 2009 was found for some of the lake's bottom, with more areas associated with bottom elevation increases than decreases. The changes and inter-annual variability in the bottom topography were attributed to the combined effect of human activities (e.g., sand dredging and levee construction) and weather events. One example was the increased bottom elevation from 2002 to 2003, which was apparently due to the excessive precipitation in 2002 and the impoundment of the Three-Gorges Dam in 2003. The 10-year record of the bottom topography of this highly dynamic lake provides baseline information to monitor the impact of future engineering and management activities, to estimate the lake's water and sediment budgets, and to aid ship navigation. (C) 2011 Elsevier Inc. All rights reserved.
引用
收藏
页码:2729 / 2741
页数:13
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