Timelapse footage of the classic appearance of clouds on the downslope of a mountain range. As warm moist air is lifted by a mountain, clouds condense as it rises and cools, forming clouds that end abruptly, known as a foehn wall. Lenticular clouds can also develop (as at centre right), which form at the top of the air's movement. These clouds remain in the same place, with the wind blowing through them. Filmed in the USA in autumn in the afternoon.
Details
WebID:
C01834567
Clip Type:
RF
Super High Res Size:
1920X1080
Duration:
00:00:31.000
Format:
QuickTime
Bit Rate:
29 fps
Available:
download
Comp:
200X112 (0.00 M)
Model Release:
NO
Property Release
NO