Snowy mountain with valley fog below, due to a temperature inversion. An inversion is where the normal cooling of the air with altitude is replaced by warmer air above a layer of cold dense air. With sufficient humidity, fog can form in the cold layer and persist for a long time. Filmed from Red Screes, above Ambleside, Lake District, UK. | |
Licence : | Droits gérés |
Crédit : | Science Photo Library / Cooper, Ashley |
Model Release : | Non requis |
Durée : | 19 Secondes |
Aspect ratio : | 16/9 |
Restrictions : | - |