基于遥感的山区河流“断面-河段”形态特征分析

    Remote sensing-based analysis of cross-section-reach morphological characteristics in mountainous rivers

    • 摘要: 山区河道断面形态及其组合特征是基于遥感的河道径流测算、区域河流生态治理、防洪治理等的重要基础。基于遥感数据提取山区河流水面矢量文件,搭建断面形态特征指标体系,通过k均值聚类方法识别断面、河段分类特征及其组合分类特征。结果显示:金沙江上段断面形态可分为5类,其中对称峡谷控制段(0类)占比76.98%,形态特征与水动力环境显著关联;河段形态复杂度随长度增加而上升(300m至1500m河段聚类类别增至19类),短河段以单一动力过程主导,长河段受地形-水流交互作用影响显著。枯汛期水面宽比均值0.52,汛期水流右偏(rx均值1.18),与科氏力效应吻合。研究结果可以为基于遥感的缺资料地区径流测算、山区河流水动力模拟、生态修复及防洪管理、应急监测条件下应急监测点位快速识别等提供科学依据。

       

      Abstract: The morphological characteristics and compositional patterns of cross-sections in mountainous river channels constitute a fundamental basis for remote sensing-based runoff estimation, regional riverine ecological management, and flood control strategies. In this study, water surface vector files of mountainous rivers were extracted from remote sensing data, upon which a comprehensive index system for cross-sectional morphological features was constructed. Using the K-means clustering method, we identified classifications of individual cross-sections, river reaches, and their combined morphological assemblages.The results indicate that the upper reaches of the Jinsha River exhibit five distinct types of cross-sectional morphology. Among them, the symmetric gorge-controlled type (Category 0) dominates, accounting for 76.98%, and shows a strong correlation with the prevailing hydrodynamic conditions. Furthermore, the complexity of river reach morphology increases with reach length; clustering categories rise from 5 to 19 as reach lengths extend from 300 m to 1500 m. Short reaches tend to be governed by singular hydrodynamic processes, while longer reaches are significantly influenced by topographic–hydrologic interactions.During the dry and flood seasons, the mean ratio of low-flow to high-flow water surface width is 0.52. In the flood season, a rightward flow deviation is observed (mean right-bias index rx = 1.18), consistent with the Coriolis effect. These findings provide scientific support for runoff estimation in data-scarce regions using remote sensing, hydrodynamic simulation in mountainous rivers, ecological restoration and flood risk management, as well as rapid identification of monitoring sites under emergency monitoring scenarios.

       

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