河道主ADCP与RiverSonde雷达测量河道流量的现场比对

P. Spain, R. Marsden, D. Barrick, C. Teague, C. Ruhl
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引用次数: 2

摘要

RiverSonde雷达可以非接触式测量河段的水平面速度。这种雷达已经在美国西部的几条河流上成功地工作了,它显示出与声波传播时系统记录的同一水平上的平均水流同时测量的令人鼓舞的相关性。这项工作报告了一项实地研究,将来自600 kHz信道主ADCP的数据集与RiverSonde雷达进行比较。主要目标是开始探索雷达数据作为可靠的放电指标的稳健性。这个地点位于美国加州北部的三里沼泽。这项工作的更大目的是检查雷达的地表水流与穿越河段的地下水流在空间和时间上的变化。这里我们检查了几个强风时期的数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Field intercomparison of Channel Master ADCP with RiverSonde radar for measuring river discharge
The RiverSonde radar makes non-contact measurement of a horizontal swath of surface velocity across a river section. This radar, which has worked successfully at several rivers in the western USA, has shown encouraging correlation with simultaneous measurements of average currents at one level recorded by an acoustic travel-time system. This work reports a field study intercomparing data sets from a 600 kHz Channel Master ADCP with the RiverSonde radar. The primary goal was to begin to explore the robustness of the radar data as a reliable index of discharge. This site is at Three Mile Slough in northern California, USA. The larger intent of the work is to examine variability in space and time of the radar's surface currents compared with subsurface flows across the river section. Here we examine data from a couple of periods with strong winds.
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