Timelapse footage of intense gravity waves propagating through a layer of stratocumulus clouds. This is occurring at a frontal boundary, where warm air has moved over colder, denser air, forming a temperature inversion. The boundary between the cold dense air and the warmer air above it displays waves analogous to those seen when wind blows over a water surface. Filmed in the USA on a summer afternoon. | |
Licence : | Libre de droits |
Crédit : | Science Photo Library / Weathervideohd.tv |
Model Release : | Non requis |
Property release : | Non requis |
Durée : | 20 Secondes |
Aspect ratio : | 16/9 |
Restrictions : | - |