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首页> 外文期刊>Quaternary International >Analysis of lengths, water areas and volumes of the Three Gorges Reservoir at different water levels using Landsat images and SRTM DEM data
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Analysis of lengths, water areas and volumes of the Three Gorges Reservoir at different water levels using Landsat images and SRTM DEM data

机译:使用Landsat图像和SRTM DEM数据分析不同水位的三峡水库的长度,水域和容量

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摘要

The impoundment and operation of the Three Gorges Reservoir (TGR) are geophysical "controlled experiments". However, detailed procedures, data source and uncertainties on TGR's basic parameters, such as lengths, water areas and volumes, were not available to the science community, and are provided in this study by using Landsat images, SRTM DEM data and in situ measurements. Reservoir lengths are between 650 km and 700 km at the water level of 175 m above sea level (a.s.l.). The natural (but near maximum) water area of the Yangtze River within the reservoir (at the full range of 699 km) based on Landsat images was 489 km~2 in August, 2002, before the impoundment. At 175 m a.s.l., the total water area mapped by Landsat images (929 km2) is ~10% less than those derived from SRTM DEM data (1006 km~2) and reported by Three Gorges Corporation (TGC) (1040 km~2). SRTM DEM data could classify 90-92% of these areas as water areas, while the total areas from Landsat, SRTM and TGC have over 96% agreements at water levels <170 m. The larger estimate of water area by DEM data from both TGC and SRTM at 175 m could be partially explained by the construction of levees. The total static volumes derived from SRTM DEM data above 70 m have a linear relationship [R~2 = 0.99, Mean Absolute Difference = 0.43 km~3) with those reported by the Information Center of Water Resource (ICWR), Ministry of Water Resource, China. The analysis also suggests that the ICWR-reported water volumes in the reservoir neglect the wedge storage in a flooding peak.
机译:三峡水库(TGR)的蓄水和运行是地球物理的“受控实验”。但是,科学界尚无法获得有关TGR基本参数(例如长度,水域和体积)的详细程序,数据源和不确定性,而本研究通过使用Landsat图像,SRTM DEM数据和现场测量来提供这些详细信息。在海拔175 m(a.s.l.)的水位处,水库长度在650 km至700 km之间。根据Landsat影像,在蓄水之前,2002年8月,长江水库(全程699 km)内长江的自然(但接近最大)水域为489 km〜2。在175 m asl时,Landsat影像绘制的总水域面积(929 km2)比三峡公司(TGC)报告的SRTM DEM数据(1006 km〜2)少10%(1040 km〜2)。 。 SRTM DEM数据可以将这些地区的90-92%归为水域,而Landsat,SRTM和TGC的总面积在水位<170 m时有超过96%的协议。 TGC和SRTM在175 m处通过DEM数据得出的更大的水域面积估计可以部分由堤坝的建设来解释。从70m以上的SRTM DEM数据得出的总静体积与水利部水利信息中心(ICWR)报告的静体积具有线性关系[R〜2 = 0.99,平均绝对差= 0.43 km〜3)。 ,中国。分析还表明,ICWR报告的水库中的水量忽略了洪峰中的楔形水库。

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  • 来源
    《Quaternary International》 |2013年第5期|115-125|共11页
  • 作者单位

    Center of Integrated Geographic Information Analysis, School of Geography and Planning, and Guangdong Key Laboratory for Urbanization and Geo-simulation, Sun Vat-sen University, 135 West Xingang Road, Guangzhou, Guangdong 510275, China;

    Center of Integrated Geographic Information Analysis, School of Geography and Planning, and Guangdong Key Laboratory for Urbanization and Geo-simulation, Sun Vat-sen University, 135 West Xingang Road, Guangzhou, Guangdong 510275, China;

    National Climate Centre, China Meteorological Administration, Beijing, China;

    National Climate Centre, China Meteorological Administration, Beijing, China;

    Laboratory of Remote Sensing and Geoinformatics, Department of Geological Sciences, University of Texas at San Antonio, TX, USA;

    Center of Integrated Geographic Information Analysis, School of Geography and Planning, and Guangdong Key Laboratory for Urbanization and Geo-simulation, Sun Vat-sen University, 135 West Xingang Road, Guangzhou, Guangdong 510275, China,Department of Geography, University of Cincinnati, Cincinnati, OH, USA;

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