Pembekuan hujan: Perbedaan antara revisi

'''FreezingHujan rainbeku''' is({{lang-en|freezing therain}}) nameadalah givennama toyang diberikan untuk [[rainhujan]] thatyang fallsturun when surface temperatures are belowketika [[melting pointtemperatur|freezingsuhu]]. hujan Unlikedi bawah [[raintitik and snow mixedleleh]], [[iceatau pellets]],panas. orTidak seperti [[hailhujan es]];, freezinghujan rainbeku isdibuat madeseluruhnya entirelydari oftetesan liquid droplets[[cair]]. TheHujan raindropsini becomemenjadi [[supercooling|supercooled]]sangat whiledingin passingketika throughmelewati asebuah lapisan ''sub-freezing'' layerdari ofudara air manyratusan-ribuan hundreds ofkaki feetdi aboveatas thepermukaan surfacetanah, anddan thenkemudian [[freezingPembekuan|freezemembeku]] upondi atas impactdampak withdengan anyobjek objectapapun theyyang encounterdihadapi.<ref>Glossary of Meteorology. [http://amsglossary.allenpress.com/glossary/browse?s=f&p=39 F.] {{Webarchive|url=https://web.archive.org/web/20070807032832/http://amsglossary.allenpress.com/glossary/browse?s=f&p=39 |date=2007-08-07 }} Retrieved on 2008-02-17.</ref> TheHasilnya, resultingdalam ice,bentuk calledes disebut [[:en:glaze ice|glazeglasir]], candapat accumulateterakumulasi todengan aketebalan thicknessbeberapa of several centimeters[[sentimeter]]. TheKode [[METAR]] codeuntuk for freezing rain{{PAGENAME}} isadalah '''FZRA'''.

== Lihat pula ==

* [[Presipitasi|Curah hujan]]