Ground Fog

German: Bodennebel

A thin blanket of fog hugging the surface while the sky above stays clear. Most common in autumn pre-dawn hours.

Ground Fog - photography example

Ground fog creates an ethereal, otherworldly atmosphere - a thin blanket hugging the surface while everything above stays clear. It forms when humidity is very high (90%+), wind is nearly calm, and the air temperature drops close to the dew point. These conditions are most common in autumn and early winter during the pre-dawn hours.

Inverza watches for the triple convergence of high humidity, low wind speed, and a minimal temperature-dew point gap. Calmer winds and tighter temperature gaps score higher, as they indicate denser, more stable fog formation.

Tip: Get to an elevated viewpoint to shoot down into the fog. Trees and buildings poking through the fog layer create a mystical 'floating' effect. Combine with sunrise for warm light filtering through the mist.

Frequently asked

When is ground fog most likely?

Autumn and early winter mornings in the hour before sunrise, when overnight radiative cooling pushes air temperature down to the dew point. It typically burns off within 1-2 hours of sunrise.

What's the difference between ground fog and a cloud inversion?

Ground fog is a thin layer right at the surface. A cloud inversion is a deeper layer of cloud trapped in valleys by a temperature inversion, with ridges poking above it. Inverza detects both separately.

Inverza detects every condition above automatically. Set your location and get notified when something special is coming.

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