Freezing rain - Wikipedia
Freezing rain is rain maintained at temperatures below freezing by the ambient air mass that causes freezing on contact with surfaces. Unlike a mixture of rain and snow or ice pellets, freezing rain is made entirely of liquid droplets.
Freezing rain: All about this dangerous ice - EarthSky
2023年1月26日 · Freezing rain is simply rain that falls through a shallow layer of cold temperatures at or below 32 degrees F (0 degrees Celsius) near the surface. When this rain becomes super-cooled, it...
冻雨 - 百度百科
冻雨（freezing rain）是由过冷水滴组成。 当它在降落过程中遇到温度低于摄氏零度的物体，迅速冻结成冰的降水现象。 冻雨通常发生在初冬和冬末春初时节。
Freezing Rain and Sleet - National Weather Service
Freezing rain occurs when the layer of freezing air is so thin that the raindrops do not have enough time to freeze before reaching the ground. Instead, the water freezes on contact with the surface, creating a coating of ice on whatever the raindrops contact.
冻雨 - 维基百科，自由的百科全书
冻雨（英語：Freezing rain）是0℃以下的過冷雨滴落於地面時，迅速凝結為冰的一种特殊降水現象 [1] 。冻雨通常發生於地面溫度0℃以下的天气情况，特别是在初冬和初春和时节。在航空例行天氣報告（METAR）中，冻雨现象的代码是“FZRA”。 [2]
Freezing Rain Definition - ThoughtCo
2019年7月24日 · Freezing rain happens when precipitation falls as liquid raindrops, then freezes as it hits individual objects on the ground whose temperatures are below 32 degrees Fahrenheit. The ice that results is called glaze ice because it covers the objects in a smooth coating.
Five Reasons Why Freezing Rain Really Is The Worst
2018年11月14日 · Freezing rain occurs when the atmosphere is too warm for snow, but the ground is freezing. Freezing rain can cause major tree damage and widespread power outages.
Freezing rain - Met Office
Freezing rain is a rare type of liquid precipitation that strikes a cold surface, and freezes almost instantly. The conditions needed for freezing rain are quite specific and we don’t see this...
Freezing Rain | GLISA
Freezing rain occurs when frozen precipitation falls through a warm layer of air, causing the precipitation to melt and change from solid to liquid. However, because the surface where it lands is below freezing, the liquid precipitation freezes on contact, creating a dangerous icy layer.
凍雨 - 維基百科，自由的百科全書
凍雨 （英語：Freezing rain）是0℃以下的 過冷 雨滴落於地面時，迅速凝結為 冰 的一種特殊 降水 現象 [1]。 凍雨通常發生於地面溫度0 ℃ 以下的天氣情況，特別是在 初冬 和 初春 和時節。 在 航空例行天氣報告 （METAR）中，凍雨現象的代碼是「FZRA」。 [2] 形成原因. [編輯] 凍雨形成過程中以 雪 的形式從高空雲層落下，在下降過程中遇到溫度高於凝固點的暖氣流層而完全融化為雨滴，過冷雨滴一旦遇到低於凝固點的任何物體就會立刻凝固，形成細長條狀的冰棱，稱之為凍雨 …