Kerpasan: Perbezaan antara semakan
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Mencipta laman baru dengan kandungan 'thumb|right|340px|Long-term mean precipitation by month Dalam bidang meteorologo, '''kerpasan''' ialah hasil pemeluwapan [[wap a...' |
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[[File:MeanMonthlyP.gif|thumb|right|340px|
Dalam bidang [[
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Pertindihan kelembapan yang dikaitkan dengan [[pemuka cuaca]] ialah sebuah kaedah penghasilan kerpasan yang utama secara keseluruhannya. Jika terdapat cukup kelembapan dan gerakan ke atas, maka kerpasan turun dari awan olakan seperti [[kumulonimbus]] dan boleh tersusun menjadi [[jalur hujan]] yang tirus. Di mana adanya jasad air yang agak hangat, misalnya kesan pemeluwapan air dari tasik, maka curahan [[salji kesan tasik]] becomes a concern downwind of the warm lakes within the cold [[cyclone|cyclonic]] flow around the backside of [[extratropical cyclone]]s. Lake-effect snowfall can be locally heavy. [[Thundersnow]] is possible within a cyclone's [[Extratropical_cyclone#Surface_pressure.2FWind_distribution|comma head]] and within lake effect precipitation bands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within [[windward]] sides of the terrain at elevation. On the leeward side of mountains, desert climates can exist due to the dry air caused by compressional heating. The movement of the [[monsoon trough]], or [[intertropical convergence zone]], brings [[wet season|rainy seasons]] to [[savannah]] [[clime]]s.
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