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File:Vol d'onde.svg

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Taƙaici

Bayani Wave lift. The wind flows towards a mountain and produces a first oscillation (A). A second wave occurs farther and higher with lenticular clouds stuck on top of the flow (B). This configuration is used to access high altitudes with gliders.
Rana
Masomi Self-made illustration
Marubucin Dake

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  • dan maimaita – dan daukar aikin
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sunan mawallafi: Dake
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farawa

3 Nuwamba 2006

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Rana/LokaciWadar sufaKusurwowiMa'aikaciBahasi
na yanzu18:05, 26 ga Yuli, 2009Wadar sufa ta zubin 18:05, 26 ga Yuli, 2009369 × 270 (338 KB)PiRKThere is no amplification of the wave without resonance. Resonance only appears if there is a succession of moutains (at least 2) with a separation equal to the wavelenght of the oscillation. See file:Onde orographique avec résonance.svg.
18:18, 5 Nuwamba, 2006Wadar sufa ta zubin 18:18, 5 Nuwamba, 2006369 × 270 (177 KB)Dake~commonswiki== Description == {{Information |Description=''Wave lift''. The wind flows towards a mountain and produces a first oscillation (A). A second wave occurs farther and higher with lenticular clouds stuck on top of the flow (B). This configuration is used to

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