《Table 2.Average ice thickness, temperature, relative humidity, and wind velocity in each period of
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《"Observational Study on the Supercooled Fog Droplet Spectrum Distribution and Icing Accumulation Mechanism in Lushan, Southeast China"》
Figure 4 shows the temporal evolution of elements such as ice thickness at the 10-m height.According to the variation in ice thickness,an icing process can be divided into the icing preparation period,growth period,maintenance period,and fall-off period.Table 2 shows the ice thickness and meteorological elements for the four periods at the 10-m height.
图表编号 | XD0030264200 严禁用于非法目的 |
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绘制时间 | 2019.01.10 |
作者 | Tianshu WANG、Shengjie NIU、Jingjing Lü、Yue ZHOU |
绘制单位 | School of Atmospheric Physics,Nanjing University of Information Science and Technology、School of Atmospheric Physics,Nanjing University of Information Science and Technology、Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disa |
更多格式 | 高清、无水印(增值服务) |
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