• Adv. Atmos. Sci.  2019, Vol. 36 Issue (1): 29-40    DOI: 10.1007/s00376-018-8017-6
    Observational Study on the Supercooled Fog Droplet Spectrum Distribution and Icing Accumulation Mechanism in Lushan, Southeast China
    Tianshu WANG1, Shengjie NIU1, 2, 3, *(), Jingjing Lü1, 4, Yue ZHOU5
    1School of Atmospheric Physics, Nanjing University of Information Science and Technology, Nanjing 210044, China
    2Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing 210044, China
    3Nanjing Tech University, Nanjing 211816, China
    4Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science and Technology, Nanjing 210044, China
    5Wuhan Regional Climate Center, Wuhan 430074, China
    Abstract
    Abstract  

    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 January 2016, 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.

    Corresponding Authors: Shengjie NIU   
    Just Accepted Date: 03 September 2018   Issue Date: 01 November 2018
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    Tianshu WANG
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    Yue ZHOU
    Cite this article:   
    Tianshu WANG,Shengjie NIU,Jingjing Lü, et al. Observational Study on the Supercooled Fog Droplet Spectrum Distribution and Icing Accumulation Mechanism in Lushan, Southeast China[J]. Adv. Atmos. Sci., 2019, 36(1): 29 -40 .
    URL:  
    http://159.226.119.58/aas/EN/10.1007/s00376-018-8017-6     OR     
    http://159.226.119.58/aas/EN/Y2019/V36/I1/29
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