吴剑平, 杜洪波, 李文杰, 万宇, 肖毅, 杨胜发. 基于遥感数据的山区河流测深反演方法与应用[J]. 水科学进展, 2023, 34(5): 766-775. DOI: 10.14042/j.cnki.32.1309.2023.05.011
引用本文: 吴剑平, 杜洪波, 李文杰, 万宇, 肖毅, 杨胜发. 基于遥感数据的山区河流测深反演方法与应用[J]. 水科学进展, 2023, 34(5): 766-775. DOI: 10.14042/j.cnki.32.1309.2023.05.011
WU Jianping, DU Hongbo, LI Wenjie, WAN Yu, XIAO Yi, YANG Shengfa. Mountain river bathymetry inversion method based on remote sensing data and its application[J]. Advances in Water Science, 2023, 34(5): 766-775. DOI: 10.14042/j.cnki.32.1309.2023.05.011
Citation: WU Jianping, DU Hongbo, LI Wenjie, WAN Yu, XIAO Yi, YANG Shengfa. Mountain river bathymetry inversion method based on remote sensing data and its application[J]. Advances in Water Science, 2023, 34(5): 766-775. DOI: 10.14042/j.cnki.32.1309.2023.05.011

基于遥感数据的山区河流测深反演方法与应用

Mountain river bathymetry inversion method based on remote sensing data and its application

  • 摘要: 河流测深是河流研究中的重要基础数据, 但受地形交通条件限制山区河流测深数据匮乏, 遥感监测技术为测深反演提供了新途径。本文基于河道概化断面推导水位—河宽理论关系, 结合Hydroweb数据集和Sentinel-1影像提出河流测深反演方法, 分析暴露水平、河段平均长度、遥感观测误差因素对反演精度的影响, 应用于长江上游, 以验证该方法模拟河流流量的潜力。研究结果表明: ①河床高程估算误差为4.00~4.06 m, 估算断面占实际断面面积达73.69%~80.29%, 反演效果相对较好。②暴露水平是影响反演精度的主要因素, 与反演精度呈正相关关系; 选择合适的河段平均长度可改善反演效果, 建议长江上游选取10 km; 相较河宽, 反演精度对水位遥感观测误差更为敏感。③采用该方法估算河流流量效果较好, 纳什效率系数达0.92, 具备推广应用潜力。研究成果可为无(缺)资料区河流测深监测提供新的解决思路。

     

    Abstract: River bathymetry (RB) is a fundamental dataset in the field of river research. However, mountainous regions often lack comprehensive data due to topographical and transportation challenges. Remote sensing technology provides an innovative method for estimating RB. In this study, the theoretical relationship between the water level and the river width is established by generalizing the channel cross-section shape. A novel RB estimation method was proposed, integrating the Hydroweb dataset and Sentinel-1 images. The impacts of exposure, reach-average length, and remote sensing observation errors on estimation accuracy were systematically analyzed. The method was applied to the Upper Yangtze River to evaluate its potential for estimating river discharge. Results reveal that: ① The estimation error of the riverbed elevation ranges from 4.00 m to 4.06 m, with the estimated cross-section representing 73.69% to 80.29% of the actual area, indicating precise RB estimation. ② Exposure rate emerges as a primary factor, significantly enhancing estimation accuracy. An appropriate reach-average length improves the estimation precision and optimal length of 10km is advised for the Upper Yangtze River. Furthermore, the accuracy of RB estimation is more susceptible to water level errors in remote sensing than to river width. ③ The method demonstrates the potential to estimate river discharge achieving a Nash efficiency coefficient of 0.92. The research outcome can provide a novel approach to RB monitoring in data-scarce regions.

     

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