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Experimental Studies of Icing Resistanceand Observation of Icing Sleet in Heavy Icing Areaat Huangmaogeng Icing Observation Station
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作者 LiuYu XiongHaixing ChangZhineng 《Electricity》 1999年第4期35-37,共3页
关键词 Experimental Studies of icing Resistanceand observation of icing Sleet in Heavy icing Areaat Huangmaogeng icing observation Station
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Observational Study on the Supercooled Fog Droplet Spectrum Distribution and Icing Accumulation Mechanism in Lushan, Southeast China 被引量:4
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作者 Tianshu WANG Shengjie NIU +1 位作者 Jingjing Lü Yue ZHOU 《Advances in Atmospheric Sciences》 SCIE CAS CSCD 2019年第1期29-40,共12页
A fog monitor, hotplate total precipitation sensor, weather identifier and visibility sensor, ultrasonic wind speed meter,an icing gradient observation frame, and an automated weather station were involved in the obse... A fog monitor, hotplate total precipitation sensor, weather identifier and visibility sensor, ultrasonic wind speed meter,an icing gradient observation frame, and an automated weather station were involved in the observations at the Lushan Meteorological Bureau of Jiangxi Province, China. In this study, for the icing process under a cold surge from 20–25 January2016, the duration, frequency, and spectrum distribution of agglomerate fog were analyzed. The effects of rain, snow, and supercooled fog on icing growth were studied and the icing and meteorological conditions at two heights(10 m and 1.5 m)were compared. There were 218 agglomerate fogs in this icing process, of which agglomerate fogs with durations less than and greater than 10 min accounted for 91.3% and 8.7%, respectively. The average time interval was 10.3 min. The fog droplet number concentration for sizes 2–15 μm and 30–50 μm increased during rainfall, and that for 2–27 μm decreased during snowfall. Icing grew rapidly(1.3 mm h-1) in the freezing rain phase but slowly(0.1 mm h-1) during the dry snow phase. Intensive supercooled fog, lower temperatures and increased wind speed all favored icing growth during dry snow(0.5 mm h-1). There were significant differences in the thickness, duration, density, and growth mechanism of icing at the heights of 10 m and 1.5 m. Differences in temperature and wind speed between the two heights were the main reasons for the differences in icing conditions, which indicated that icing was strongly affected by height. 展开更多
关键词 cold surge microstructure of supercooled fog icing gradient observation growth rate of icing
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