Fog generated when winds flow over a surface with a different temperature. Two types of advection fog exist. When warm air flows over a cold surface it can produce fog through contact cooling. Cold ai [..]

A fog that forms when warm air flows over a cold surface and cools from below until saturation is reached.

Occurs when warm, moist air moves over a cold surface and the air cools to below its dew point.

water vapor that condenses as warm, moist air passes over a cool surface.

A type of fog caused by the advection of moist air over a cold surface, and the consequent cooling of that air to below its dewpoint. A very common advection fog is that caused by moist air over a col [..]

A type of fog formed when warm, moist air moves ?horizontally over a cold surface and the air is consequently cooled to below its dew point; this is found especially along a coastline where the temperature of land and the temperature of water markedly differ.

Fog formed by warm, humid air flowing over colder surface

Can occur any time warm, moist air blows over a surface cool enough to drop it's temperature below the dew point.

Can occur any time warm, moist air blows over a surface cool enough to drop it's temperature below the dew point.

Fog that forms as warmer, moist air moves over a cold ground. The air is cooled to saturation by the loss of heat to the cold ground. Unlike radiation fog, advection fog may form under cloudy skies and with moderate to strong winds. Initial stability is relatively unimportant since low level cooling makes the air unstable near the ground.

a fog

Of or pertaining to the operation or navigation of aircraft.

Fog resulting from the transport of warm, humid air over a cold surface.

A fog that forms when warm air flows over a cold surface and cools from below until saturation is reached.

This type of fog requires horizontally moving air, or air that is advecting horizontally from one place to another. When warm and moist air blows over a cold surface, the surface cools the air. Once the air temperature cools enough to equal the dewpoint temperature, condensation is formed and creates a blanket-like thick fog formation. This describ [..]

Fog which develops when a mass of relatively warm, moist air moves over a cooler surface and cools the air below its dew point temperature. Advection fog requires movement of air to form (hence the name). Advection fog is common at sea where it is called sea fog.

Fog that develops when warm moist air moves over a colder surface, cooling that air to below its dew point.

Occurs when warm, moist air moves over a cold surface and the air cools to below its dew point.

Fog caused by the condensation of water vapour when warm, moist air crosses cold ground or sea.

Ground-level clouds generated by the cooling of a mild, humid air mass as it travels over a relatively cool surface.

a type of fog

Fog that develops when warm moist air aloft moves over a colder surface, cooling that air to below its dew point. An example is Arctic Sea Smoke, a form of sea fog.

Fog

Fog caused by warm moist air flowing over a cold surface and cooling until condensation occurs.

A fog that forms when warm air flows over a cold surface and cools from below until saturation is reached.

Fog that develops when warm moist air moves over a colder surface, cooling that air to below its dew point. Related terms: Arctic Sea Smoke and sea fog