The Impact of Wind on Precipitation Measurements from a Compact Piezoelectric Sensor

E. Chinchella, A. Cauteruccio, L. G. Lanza
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Abstract

The measurement accuracy of an electroacoustic precipitation sensor, the Vaisala WXT520, is investigated to quantify the associated wind-induced bias. The device is widely used as a noncatching tool for measuring the integral features of liquid precipitation, specifically rainfall amount and intensity. A numerical simulation using computational fluid dynamics is used to determine the bluff-body behavior of the instrument when exposed to wind. The obtained airflow velocity patterns near the sensor are initially validated in a wind tunnel. Then, the wind-induced deviation and acceleration/deceleration of individual raindrop trajectories and the resulting impact on the measured precipitation are replicated using a Lagrangian particle tracking model. The sensor’s specific measurement principle necessitates redefining catch ratios and the collection efficiency in terms of the resulting kinetic energy and quantifying them as a function of particle Reynolds number and precipitation intensity, respectively. Wind speed and direction and drop size distribution have been simulated across various combinations. The results show that the measured precipitation is overestimated by up to 400% under the influence of wind. The presented adjustment curves can be used to correct raw rainfall measurements taken by the Vaisala WXT520 in windy conditions, either in real time or as a postprocessing function. The magnitude of the adjustment at any operational aggregation level largely depends on the local rainfall and wind regimes at the site of measurement and may have a strong impact on applications in regions where wind is frequent during low- to medium-intensity precipitation.
风对紧凑型压电传感器降水测量的影响
研究了电声降水传感器 Vaisala WXT520 的测量精度,以量化风引起的相关偏差。该设备被广泛用作测量液态降水整体特征(特别是降雨量和降雨强度)的非捕捉工具。利用计算流体动力学进行的数值模拟确定了仪器在风力作用下的崖体行为。传感器附近的气流速度模式在风洞中进行了初步验证。然后,利用拉格朗日粒子跟踪模型复制风引起的单个雨滴轨迹的偏差和加速/减速,以及由此对测量降水量的影响。传感器的特定测量原理要求根据所产生的动能重新定义捕获率和收集效率,并分别将其量化为粒子雷诺数和降水强度的函数。模拟了各种组合的风速、风向和水滴大小分布。结果表明,在风的影响下,测得的降水量被高估了多达 400%。所提出的调整曲线可用于修正维萨拉 WXT520 在大风条件下测量的原始降雨量,既可实时修正,也可作为后处理功能使用。在任何操作集合级别上的调整幅度在很大程度上取决于测量地点当地的降雨和风力情况,可能会对中低强度降水期间风力频繁地区的应用产生很大影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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