《Table 4.Average ice thickness, temperature, and wind velocity in each period of wire icing at the t

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《"Observational Study on the Supercooled Fog Droplet Spectrum Distribution and Icing Accumulation Mechanism in Lushan, Southeast China"》

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Figure 7 and Table 4 compare the ice thickness and meteorological elements at the two heights.The differences in icing at the two heights were mainly manifested in four aspects.First，the ice thickness revealed a wide difference，with maximum ice thickness at 10 and 1.5 m of 20.7 and 1.2 mm，respectively；the latter was 5.8%of the former.Second，the durations of icing were quite different.The durations were102 and 61 h，respectively；icing at 1.5 m only appeared in the growth period of 10-m icing.Third，the icing density revealed wide differences；there was translucent solid ice with larger density at 1.5 m and white sponge-like ice with lower density at 10 m.Fourth，there was a difference in the icing growth mechanism.The accumulation rate of icing at 10m was closely related to factors such as the precipitation rate and microphysical characteristics of supercooled fog.The ice thickness at 1.5 m was sensitive to daily variations in temperature and relative humidity，indicating diurnal variation.