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. | |
Lizenzart: | Lizenzpflichtig |
Credit: | Science Photo Library / Cooper, Ashley |
Modell-Rechte: | nicht erforderlich |
Länge: | 19 Sekunden |
Seitenverhältnis: | 16:9 |
Restrictions: | - |