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 formed by warm, humid air moving over cooler ground or water.
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.
A type of fog caused by the flow of moist air over a cold surface, and the consequent cooling of that air to below its dew point.
Fog formed by passage of relatively warm, moist and stable air over a cool surface.
a type of fog that results from the advection of moist air over a cold surface and the cooling of the air to its dew point that follows; this type of fog is most common in coastal regions.
Occurs when warm, moist air moves over a cold surface and the air cools to below its dew point.
Fog resulting from the movement of warm, humid air over a cold surface.
Fog formed by warm, humid air flowing over colder ground or water.
Fog caused by the condensation of water vapour when warm, moist air crosses cold ground or sea.
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
A fog that forms when warm air flows over a cold surface and cools from below until saturation is reached.
a cloud of water droplets formed when warm, moist air travels over a cold surface and condenses
1. 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 cold body of water ( sea fog). 2. Sometimes applied to steam fog.
