Linked from

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

• CondensationBroader topic: Fog forms when air near the ground cools enough for condensation.

• 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.

• Cloud formationBroader topic: It forms by the same condensation or deposition processes as clouds aloft.

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

• SteamCompared with: Visible fog is liquid droplets, not gaseous steam.

• Cloud baseCompared with: Its cloud base reaches the surface, unlike an elevated cloud base.

• Stratus cloudCompared with: Stratus is essentially cloud aloft; when its base reaches the surface, conditions are called fog.

• SmogCompared with: Fog is a meteorological water-droplet phenomenon, though pollution can mix with it.

• MistCompared with: Fog is the denser visibility-reducing phenomenon distinguished from mist by convention.

• 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.

• Cloud (meteorology)Compared with: Fog has cloud-like particles but forms at ground level.

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

• Widow's BayCompared with: It similarly makes maritime setting and a community's buried history central to horror.