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首页> 外文期刊>Journal of Hydrology >High-spatial-resolution streamflow estimation at ungauged river sites or gauged sites with missing data using the National Hydrography Dataset (NHD) and US Geological Survey (USGS) streamflow data
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High-spatial-resolution streamflow estimation at ungauged river sites or gauged sites with missing data using the National Hydrography Dataset (NHD) and US Geological Survey (USGS) streamflow data

机译:Ungauged River河站点的高空间分辨率流估计或使用国家水文数据集(NHD)和美国地质调查(USGS)流数据

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摘要

The need for a method of estimating streamflow with both high-quality and high spatial resolution, particularly for ungauged sites, is critical under current circumstances: intensifying competition over water resources and limited streamgages. A source of accurate and timely computations of streamflow, particularly at high spatial resolutions, has been the National Hydrograph Dataset (NHD), a comprehensive geographic information system (GIS) dataset of vector-based surface water features such as streams, lakes, and streamgages in fine detail. Utilizing the NHD with streamflow data from the U.S. Geological Survey and usage records of local water utilities, this paper proposes a simple streamflow estimation method that computes streamflow at any point on river reaches of the NHD with valid hydrograph data and tests the method in a local 613 square mile watershed. The method assumes that linearly connecting the timings of peak or bottom-base flows from upstream to downstream hydrographs leads to retracing upstream lateral inflows that have eventually arrived at a user selected site between the upstream and downstream gauge stations of the hydrographs at any given time in a common period of record between the two hydrographs. Subsequently, the lateral inflows are added up to become the streamflow for a given site at a given time. NHD river networks and ArcGIS tools identify the locations of lateral inflows and the necessary parameters of the method. This paper assesses the results of the method by comparing them to measured streamflows through recommended evaluation statistics and visual inspection. The method has yielded promising results, including values of the Nash-Sutcliffe efficiency within 0.83 and 0.99 for daily streamflow estimates over seven years. It also credibly reconstructs missing daily streamflow over a considerable number of years.
机译:需要一种估计具有高质量和高空间分辨率的流流程的方法,特别是对于未吞吐位点,在当前情况下是至关重要的:加强水资源竞争和有限的流衬。精确和及时计算的流流量的源头,特别是在高空间分辨率,是全国水文编程数据集(NHD),一种综合的地理信息系统(GIS)基于矢量的地表水分,如流,湖泊和流衬细节细节。利用来自美国地质调查和使用本地水实用程序的使用记录的NHD,提出了一种简单的StreamFlow估计方法,可在NHD的任何点上使用有效的水编辑数据计算流流程,并在本地测试该方法613平方英里的水域。该方法假设线性连接从上游到下游水位的峰值或底部基础的定时导致回到最终到达在任何给定时间的文化照片的上游和下游计量站之间的用户所选地点的上游横向流入两种水文之间的常见记录。随后,加入横向流入以在给定时间成为给定站点的流流。 NHD River Networks和ArcGIS工具识别横向流入的位置和该方法的必要参数。本文通过将它们与通过推荐的评估统计和目视检查进行比较来评估方法的结果。该方法产生了有希望的结果,包括在0.83和0.99内的NASH-SUTCLIFFE效率的值,用于每日流流估计超过七年。它也可靠地重建在相当数年内缺少日常流流。

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