Inversions trap fog in valleys and create the sea-of-clouds effect photographers drive hours to shoot. LightCast FogCast factors inversion conditions into its fog probability and burn-off timing.
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Normally, air gets colder as you gain altitude. A temperature inversion reverses this: a layer of warm air sits above cooler surface air, acting as a lid. The cold air below can't rise and mix, so any moisture or fog it holds stays locked in place. For photographers, this is what creates the valley fog and sea-of-clouds conditions visible from ridges and peaks.
A strong overnight inversion raises fog formation probability by concentrating cold, moist air at the surface. It also extends the fog duration by preventing mixing after sunrise. FogCast combines inversion conditions with dew point depression, overnight wind, recent precipitation, and terrain to give you a single probability score and estimated formation and burn-off window for your location.
Fog probability ยท Inversion conditions ยท Formation & burn-off timing
7-day outlook ยท Terrain-aware ยท Saved locations
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