melting-layer 零度层亮带
re-melting layer 重熔层
partial melting layer 部分熔融层
melting layer of precipitation 降雨融化层
reasonable thickness of melting layer 融化层的合理厚度
melting surface layer 熔化的表面层
Peak value of 2D-P mean diameter, maximum and peak diameter is corresponding with radar bright band echoes around the melting layer.
在融化层附近，2D-P观测到的粒子的平均直径、最大直径、峰值直径的峰值集中在此范围内，与融化层回波亮带对应。
参考来源 - 一次典型层状云降水物理特征的观测和数值模拟研究·2,447,543篇论文数据，部分数据来源于NoteExpress
The principle and methods to determine the reasonable thickness of melting layer and stope area are introduced here emphatically.
文中还着重介绍了融化层合理厚度和所必须采场面积的确定原则和方法。
The results show that, the stable and thicker melting layer and cold layer in low level was direct cause of exist the wide range of freezing rain.
结果表明，深厚而稳定的逆温层和低空冷层的存在是大范围冻雨出现的直接原因。
The results show that the water vapor convergence and the strong upward movement between the freezing layer and the melting layer are the essential conditions for the formation of freezing rain.
结果表明，冻结层和融化层之间的水汽辐合和较强的上升运动是冻雨产生的两个必要条件。
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