首页> 外文期刊>International journal of remote sensing >Remote sensing-based river discharge estimation for a small river flowing over the high mountain regions of the Tibetan Plateau
【24h】

Remote sensing-based river discharge estimation for a small river flowing over the high mountain regions of the Tibetan Plateau

机译:藏高山地高原流动的小型河流的遥感河蓄估计

获取原文
获取原文并翻译 | 示例
           

摘要

River discharge, as one of the most essential climate variables, plays a vital role in the water cycle. Small-scale headwater catchments including high-mountain regions of Tibetan Plateau (TP) Rivers are mostly ungauged. Satellite technology shows its potential to fill this gap with a high correlation of satellite-derived effective river width and corresponding in-situ gauged discharge. This study is innovative in estimating daily river discharge using modified Manning equation (Model 1), Bjerklie equation (Model 2), and Rating curve approach (Model 3) by combining river surface hydraulic variables directly derived from remote-sensing datasets with other variables indirectly derived from empirical equations, which greatly contributes to the improvement of river flow measurement information especially over small rivers of TP. We extracted the effective width from Landsat image and flow depth via hydraulic geometry approach. All the input parameters directly or indirectly derived from remote sensing were combined and substituted into the fundamental flow equations/models to estimate discharges of Lhasa River. The validation of all three models' results against the in-situ discharge measurements shows a strong correlation (the Nash-Sutcliffe efficiency coefficient (NSE) and the coefficient of determination (R-2) values = 0.993), indicating the potentiality of the models in accurately estimating daily river discharges. Trends of an overestimation of discharge by Model 1 and underestimation by Model 2 are observed. The discharge estimation by using Model 3 outperforms Model 1 and Model 2 due to the uncertainties associated with the estimation of input parameters in the other two models. Generally, our discharge estimation methodology performs well and shows a superior result as compared with previously developed multivariate empirical equations and its application for other places globally can be the focus of upcoming studies.
机译:作为最重要的气候变量之一,河流放电在水循环中起着至关重要的作用。包括藏高高原(TP)河流的小山地地区大部分都是未凝固的。卫星技术表明其填补这种差距的潜力,卫星衍生的有效河流宽度和对应的原位测量放电。本研究在使用修改的曼宁方程(模型1),Bjerklie等式(模型2)和评级曲线方法(型号3)通过间接与其他变量与其他变量直接导出的河流表面液压变量组合来估计日常河流放电源自经验方程,这极大地有助于改善河流测量信息,尤其是TP的小河流。我们通过液压几何方法从Landsat图像和流量深度提取有效宽度。将遥感直接或间接导出的所有输入参数组合并被替换为基本流动方程/模型以估算拉萨河的排放。所有三种模型对原位放电测量的结果的验证表明了强烈的相关性(NASH-SUTCLIFFE效率系数(NSE)和确定系数(R-2)值> = 0.993),表明潜在的潜力准确估算日河排放的模型。观察到通过模型1和模型2低估了放电过度估计的趋势。由于与其他两个模型中的输入参数相关联的不确定性,通过使用模型3优于型号1和模型2的放电估计。通常,我们的放电估计方法表现良好,并且与先前显影的多元经验方程相比,其对全球其他地方的应用是即将到来的研究的重点。

著录项

  • 来源
    《International journal of remote sensing》 |2020年第10期|3322-3345|共24页
  • 作者单位

    Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes & Land Surface P Beijing Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci Beijing Peoples R China|Univ Chinese Acad Sci Beijing Peoples R China|Arba Minch Univ Fac Meteorol & Hydrol Water Technol Inst Arba Minch Ethiopia;

    Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes & Land Surface P Beijing Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci Beijing Peoples R China|Univ Chinese Acad Sci Beijing Peoples R China;

    Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Tibetan Environm Changes & Land Surface P Beijing Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci Beijing Peoples R China;

    Minist Water Resources Informat Ctr Beijing Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号