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A snow accretion simulation method considering precipitation types based on the liquid water fraction of falling snowflakes

机译:一种基于落雪花液体水分的降水类型的雪增蚀仿真方法

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A numerical model for evaluating liquid water fraction of falling snowflakes is presented and is implemented into a snow accretion simulation code for overhead transmission lines,named SNOVAL(R)R(Ver.3).The new model allows to predict surface precipitation types(dry snow,wet snow,and rain)from averaged value of liquid water fraction of snowflakes with different size and density.It is shown that the averaged liquid water fraction of melting snowflakes depends not only on surface air temperature and relative humidity but also on the vertical temperature profile and precipitation intensity.By comparing temporal changes of observed snow load accreted on conductor samples with those of calculated liquid water fraction of snowflakes,it is found that snow accretion starts when the liquid water fraction is less than approximately 0.5.This condition based on the liquid water fraction is more accurate than using temperature or wet bulb temperature.
机译:提出了一种评价落雪花液体水分的数值模型,并实现成架空传输线的雪增值仿真码,命名为Snoval(R)R(Ver.3)。新型号允许预测表面沉淀类型(干燥从具有不同尺寸和密度的雪花液体水分的平均值的雪,湿雪和雨)。表明熔融雪花的平均液体水分不仅取决于表面空气温度和相对湿度,还取决于垂直温度曲线和降水强度。比较观察到的雪地载体的时间变化与雪花的计算液体水分分数的导体样品上的散热器样品的时间变化,发现液体水分馏分小于约0.5时开始散雪。该条件基于液体水分馏分比使用温度或湿灯泡温度更精确。

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