Whether you call it radiation fog, ground fog, valley fog or a temperature inversion, it all comes down to the same physics: the atmosphere flipping upside down. CBC’s Johanna Wagstaffe breaks down how a high-pressure system can turn our valleys into bowls of clouds.
Breakdown
- Fog forms when cold, heavy air settles at ground level, creating an inversion. 23s
- High pressure can trap air and moisture, leading to fog formation. 30s
- Fog is most common in the morning due to overnight ground cooling. 42s
- The fog layer is usually shallow, from 50 to a few hundred meters thick. 56s
- Fog can cause whiteout at ground level while higher elevations remain clear. 1m 0s