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Monitoring of Flooded Area and Water-Volume in Large Lake using Remote sensing/GIS Technology.---A Case Study of Dongting Lake in Changjiang River Basin---

机译:利用遥感/ GIS技术监测大型湖水中的洪水区和水量.--------江河流域洞庭湖的案例研究 -

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By using Terra/MODIS satellite images and ground measured water level data in 2002, the dynamic variation of surface water area and water storage in Dongting Lake (Changjiang River Basin, China) was studied. Recently, middle reaches of Changjiang River faces a serious disaster caused by large flooding, which have resulted from cumulative impacts of excessive development in the upper stream. In order to mitigate the flooding and evaluate potential flood alleviation around Dongting Lake flooded, it is necessary to estimate the water volume of Dongting Lake using satellite based monitoring technology. We, at first, divided the whole Dongting Lake into three parts (WDL: West Dongting Lake, SDL: South Dongting Lake, EDL: East Dongting Lake from west side) based on geographical characteristics. Secondly, surface water area was detected according to spectral deference between water and terrestrial area using Terra/MODIS Vegetation-Index (VI) products (Level 3-16 Day). The time interval of monitoring period was 16 days. Thirdly, the surface water area was overlaid on the lake bottom DEM with a grid size of 50m by 50m so that the water level could be calculated. Finally the water storage was obtained by times relevant water depth (difference between water surface elevation and lake-bottom elevation.) with the grid area. The total water storage at Dongting Lake was calculated by accumulating all water column values in the whole lake. By comparing the estimated water level and storage with the measurements in the three parts of the Dongting Lake, we found that there are high correspondences between the two, which implies that our method is an effective approach to estimate water level and water storage of a large lake.
机译:通过2002年使用Terra / Modis卫星图像和地面测量的水位数据,研究了Dongting Lake(ChangJiang River Bourin)的地表水域和储水的动态变化。最近,长江中游面临着大型洪水引起的严重灾难,这导致了上游过度发展的累积影响。为了减轻洪水湖洪水周围的洪水和评估潜在的洪水缓解,有必要使用基于卫星的监测技术来估算洞庭湖的水量​​。首先,我们将整个洞庭湖分为三个部分(WDL:West Dongting Lake,SDL:South Dongting Lake,EDL:来自西侧的东洞庭湖)基于地理特征。其次,根据水和陆地面积之间的光谱偏移使用Terra / Modis植被指数(VI)产品(3-16天)来检测地表水域。监测期的时间间隔为16天。第三,地表水域在湖底DEM上覆盖,电网尺寸为50米,使水位可以计算。最后,储水是通过相关的水深(水面升高和湖底高度差异之间的差异。洞庭湖的总储水量通过在整个湖泊中积累所有水柱值来计算。通过将估计的水位和储存与洞庭湖三个部分的测量进行比较,我们发现两者之间存在高的对应关系,这意味着我们的方法是估计水位和储水的有效方法湖。

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