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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Discharge estimation in high-mountain regions with improved methods using multisource remote sensing: A case study of the Upper Brahmaputra River
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Discharge estimation in high-mountain regions with improved methods using multisource remote sensing: A case study of the Upper Brahmaputra River

机译:使用Multisource遥感的改进方法的高山区域放电估计 - 胸罩上部胸罩河案例研究

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摘要

River discharge is an important variable in the water cycle that is related to water supply, irrigation, and flood forecasting. However, gauging stations are extremely limited across most high-mountain regions such as the Tibetan Plateau (TP), known as the Asia's water towers. Remote sensing, in combination with partial in situ discharge measurements, bridges the gap in monitoring river discharge over ungauged and poorly gauged basins. Of great importance for the successful retrieval of river discharge using remote sensing are river width (water surface area) and water level (water surface elevation), but it is challenging to retrieve accurate discharge values for high-mountain regions because of narrow river channels, complex terrain, and limited observations from a single satellite platform. Here, we used 1237 high-spatial-resolution images (Landsat series and Sentinel 1/2) to derive water surface areas with the Google Earth Engine (GEE), and satellite altimetry (Jason-2/3 and Satellite with Argos and AltiKa (SARAL/Altika)) to derive water levels for the Upper Brahmaputra River (UBR, the Yarlung Zangbo River in China) in the TP where the river width is typically less than 400 m. Using three power function equations, discharge was estimated for cross-sections around the four gauging stations in the UBR with triangular cross-sections outperforming their trapezoidal counterparts. It was also found that the equation combining both river width and water level produced the best discharge estimates whereas the other two equations (requiring either river width or water level as the input data) were complementary and could be used to extend the time series of discharge estimates. The Nash-Sutcliffe efficiency coefficient values for the discharge estimates range from 0.68 to 0.98 during the study period 2000-2017. The proposed method is feasible to estimate discharge in the UBR and potentially other high-mountain rivers globally.
机译:河流放电是与供水,灌溉和洪水预测有关的水循环中的一个重要变量。然而,在藏高原(TP)之类的大多数高山地区,衡量站非常有限,称为亚洲的水塔。遥感,与部分原位放电测量相结合,弥补了监测河流放电的差距,在未吞噬和较差的盆地上。使用遥感的河流放电成功检索是河流宽度(水面积)和水位(水面高度)的重要性,但由于狭窄的河流通道检索高山区域的精确放电值是挑战性的,复杂的地形,以及单个卫星平台的有限观察。在这里,我们使用了1237个高空间分辨率图像(Landsat系列和Sentinel 1/2)来使用谷歌地球发动机(Gee)和卫星Altimetry(Jason-2/3和带Argos和Altika的卫星( Saral / Altika))在TP的TP中获得上部Brahmaputra River(UBR,雅尔隆Zangbo河)的水平,河宽度通常小于400米。使用三个功率函数方程,估计UBR中的四个测量站周围的横截面的放电,其三角形横截面优于其梯形对应物。还发现,相结合河宽度和水位的等式产生了最佳的放电估计,而另外两个方程式(需要河宽或作为输入数据的水位)是互补的,可用于延长排出的时间序列估计。在研究期间,在2000-2017期间,排放估计的纳什Sutcliffe的效率系数范围为0.68至0.98。所提出的方法是可行的,可以在全球估计UBR和潜在的其他高山河流中的放电。

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