Vol d'onde.svg
From WindsportAtlanta.com: Wiki
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Original file (SVG file, nominally 369 × 270 pixels, file size: 338 KB)
Summary
| 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 access high altitudes with gliders. |
| Date | |
| Source | Self-made illustration |
| Author | Dake |
Licensing
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.svg){kind=small} | This image was improved or created by the Wikigraphists of the Graphic Lab (fr). You can propose images to clean up, improve, create or translate as well. |
File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 14:05, 26 July 2009 | | 369 × 270 (338 KB) | wikimediacommons>PiRK | There 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. |
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