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Influence of systematic errors from tipping bucket rain gauges on recorded rainfall data

机译:翻斗式雨量计的系统误差对记录的降雨数据的影响

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Tipping bucket rain gauges (TBR) are widely used in urban hydrology. The present study investigated the uncertainties in recorded rainfall intensity induced by the following properties of the TBR: depth resolution i.e. the bucket volume, calibration parameters, wetting and evaporation losses and the method of data recording (time between tips or tips per minute). The errors were analysed by means of a TBR simulator i.e. a simulation program that models the behaviour of a TBR. Rainfall data disaggregated to 6 seconds from measured 1-min data and randomly varied were taken as input to the simulator. Different TBR data series were produced by changing the properties of the simulated rain gauge. These data series together with the original rainfall events were used as input to a rainfall-runoff model. Computed overflow volume and peak discharge from a combined sewer overflow (CSO) weir were compared. Errors due to depth resolution (i.e. the bucket size) proved to be small. Therefore TBRs with a depth resolution up to 0.254 mm can be used in urban hydrology without inducing significant errors. Wetting and evaporation losses caused small errors. The method of data recording had also little influence. For larger bucket volumes variable time step recording induced smaller errors than tips per minute recording. (C) 1998 IAWQ. Published by Elsevier Science Ltd. All rights reserved. [References: 13]
机译:自卸车雨量计(TBR)在城市水文学中被广泛使用。本研究调查了由TBR的以下特性引起的记录的降雨强度的不确定性:深度分辨率,即铲斗体积,校准参数,润湿和蒸发损失以及数据记录方法(每小尖之间的时间或小尖之间的时间)。通过TBR仿真器(即对TBR行为进行建模的仿真程序)分析了错误。降雨数据从测得的1分钟数据中分解为6秒,然后随机变化,作为模拟器的输入。通过更改模拟雨量计的属性产生了不同的TBR数据系列。这些数据系列与原始降雨事件一起被用作降雨径流模型的输入。比较了组合下水道溢流(CSO)堰的计算溢流量和峰值流量。事实证明,由于深度分辨率(例如,铲斗尺寸)而导致的误差很小。因此,深度分辨率高达0.254 mm的TBR可以在城市水文学中使用,而不会引起明显的误差。润湿和蒸发损失引起小的误差。数据记录的方法也没有什么影响。对于较大的铲斗体积,可变的时间步距记录所产生的误差小于每分钟的吸头记录。 (C)1998 IAWQ。由Elsevier Science Ltd.出版。保留所有权利。 [参考:13]

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