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Orografiske skyer

Orografiske skyer opstår når luftmasser med meget højt vand indhold presses op i højderne på grund af topografien (landskabet) f.eks. bjergkæder. Luften der bevæger sig op ad på højere topografi (også kaldet anabatiske vinde), afkøles og vanddampene i luftmassen kondenseres således at skyer dannes. Nedbør forekommer oftest. Efter at skyerne har passeret højdepunktet, blæser vindene ned ad bjergsiden på grund af tyngdekraften (katabatiske vinde), disse medfører en mere tør luft med høj massefylde.

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