Pembekuan hujan: Perbedaan antara revisi
Konten dihapus Konten ditambahkan
Tidak ada ringkasan suntingan |
Tidak ada ringkasan suntingan |
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[[Kategori:Presipitasi]] |
[[Kategori:Presipitasi]] |
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[[Kategori:Hidrologi]] |
[[Kategori:Hidrologi]] |
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[[af:Vriesreën]] |
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[[da:Isslag]] |
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[[de:Regen#Gefrierender Regen]] |
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[[En:Freezing rain]] |
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[[es:Lluvia congelada]] |
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[[eo:Frostiĝanta pluvo]] |
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[[eu:Euri izoztua]] |
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[[fr:Pluie verglaçante]] |
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[[it:Pioggia congelantesi]] |
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[[lv:Atkala]] |
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[[lt:Lijundra]] |
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[[hu:Ónos eső]] |
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[[nds-nl:Iesel (weer)]] |
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[[ja:雨氷]] |
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[[no:Underkjølt regn]] |
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[[nn:Underkjølt regn]] |
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[[pl:Deszcz marznący]] |
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[[pt:Chuva congelada]] |
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[[ro:Ploaie înghețată]] |
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[[ru:Гололёд]] |
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[[sv:Frysande regn]] |
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[[uk:Ожеледь]] |
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[[zh-classical:雨冰]] |
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[[zh:冻雨]] |
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Revisi per 16 Maret 2012 11.53
 | Artikel ini perlu diterjemahkan dari bahasa Inggris ke bahasa Indonesia. |
| Bagian dari seri alam |
| Cuaca |
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Freezing rain is the name given to rain that falls when surface temperatures are below freezing. Unlike rain and snow mixed, ice pellets, or hail; freezing rain is made entirely of liquid droplets. The raindrops become supercooled while passing through a sub-freezing layer of air many hundreds of feet above the surface, and then freeze upon impact with any object they encounter.[1] The resulting ice, called glaze, can accumulate to a thickness of several centimeters. The METAR code for freezing rain is FZRA.