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Integrating Landsat Imageries and Digital Elevation Models to Infer Water Level Change in Hoover Dam

机译:整合Landsat影像和数字高程模型以推断胡佛水坝的水位变化

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The Thematic Mapper onboard Landsat 4, 5, and Enhanced Thematic Mapper Plus () onboard Landsat 7 have frequency bands (green and SWIR) to effectively measure water body extents and their changes via the Modified Normalized Difference Water Index (MNDWI). Here, we developed a technique, called the thematic imagery-altimetry system (TIAS), to infer the vertical water changes from MNDWI horizontal water extent changes by integrating long-term imageries with available digital elevation models (DEMs). The result is a technique to quantify water level changes of natural or artificial water bodies over two decades. Several DEMs were used to compute intersects with water extent time series to evaluate the robustness of the technique. These DEMs include: the Advanced Spaceborne Thermal Emission and Reflection Radiometer Global Digital Elevation Map version 2 (ASTER-GDEM2, at 1 arcsec resolution), the Shuttle Radar Topography Mission version 2 (SRTM C-band at 1 arcsec), and the Global Multiresolution Terrain Elevation Data (GMTED2010 at 7.5 arcsec). We demonstrated our technique near Hoover Dam (HD) in Lake Mead to quantify its respective decadal water level changes. The dammed water had experienced extraordinary level variation in the past 20 years due to natural decline from intake or artificial impoundments. The discrepancy of the HD water level changes from an analysis of 32-year (1984–2015) time series, including 584 Landsat scenes, using the GMTED2010 DEM, has a RMSE reached (91% of data) as compared with stage record.
机译:Landsat 4、5上的Thematic Mapper和Landsat 7上的增强型Thematic Mapper Plus()具有频带(绿色和SWIR),可通过修改后的归一化差水指数(MNDWI)有效地测量水体范围及其变化。在这里,我们开发了一种称为主题影像-测高系统(TIAS)的技术,通过将长期影像与可用的数字高程模型(DEM)集成,从MNDWI水平水位变化推断出垂直水位变化。结果是一种量化天然或人工水体在过去二十年中水位变化的技术。几个DEM用于计算水域时间序列的相交,以评估该技术的鲁棒性。这些DEM包括:先进的星载热发射和反射辐射计全球数字高程图第2版(ASTER-GDEM2,以1 arcsec分辨率),Shuttle雷达地形任务第2版(以1 arcsec的SRTM C波段)和全球多分辨率地形高程数据(GMTED2010,7.5弧秒)。我们在米德湖胡佛水坝(HD)附近展示了我们的技术,以量化其各自的年代际水位变化。由于取水量或人工蓄水量的自然下降,在过去的20年中,水位发生了异常的变化。通过使用GMTED2010 DEM对32年(1984-2015年)的时间序列进行分析(包括584个Landsat场景),高清水位变化的差异与阶段记录相比达到了RMSE(数据的91%)。

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