Linked from

The 17 pages that link to Fog, each with the reason it gives.

• Atmospheric boundary layerRelated: Stable near-surface layers can trap moisture and favor fog formation.

• Temperature inversionRelated: Surface cooling under a stable inversion can bring near-ground air to saturation.

• Dew pointRelated: Fog forms when near-surface air cools to saturation, often reaching its dew point.

• Oceanic climateRelated: Moist maritime air can produce persistent coastal fog when it cools to saturation.

• VisibilityRelated: Fog is a common cause of sharply reduced visibility at the surface.

• Great Smoky MountainsRelated: Frequent fog forms as moist air cools over the mountains.

• Sequoia sempervirensRelated: Coast redwoods intercept fog, which supplies moisture during dry summers.

• Lake MashūRelated: Fog frequently obscures Mashū's surface and surrounding crater rim.