Usually (but not always) at the coast.
Pea souper was the name given to smog (a combination of fog and smoke) which was prevalent in Britain's large cities until the mid-sixties.
Putting water in a fog machine can damage it or cause it to malfunction. Fog machines are designed to work with fog fluid, which is a specific type of liquid that gets vaporized to produce fog. Water may not produce the desired fog effect and can clog the machine's components. Always use the recommended fog fluid for your fog machine.
Thin fog is often referred to as "mist." It is a light fog that reduces visibility but is less dense than regular fog.
This type of fog is called orographic fog. It forms when moist air is lifted upslope by the terrain of the mountains. As the air rises, it cools and reaches its dew point, leading to the formation of fog.
Fog is a chemical weathering.
Usually in the damp cold of Autumn.
Fog can be especially prevalent in coastal areas, near bodies of water, and in valleys. These areas are more likely to experience fog due to the presence of moist air and temperature inversions that trap cool air near the surface.
Pea souper was the name given to smog (a combination of fog and smoke) which was prevalent in Britain's large cities until the mid-sixties.
coastal areas and valleys where there is a convergence of air masses and temperature variations. Additionally, urban areas with high levels of pollution can also experience increased fog due to the presence of particulates in the air.
Mist out at sea is commonly referred to as "sea fog" or "maritime fog." This phenomenon occurs when warm, moist air moves over cooler ocean waters, leading to condensation and the formation of fog. Sea fog can significantly reduce visibility for ships and boats, making navigation challenging. It is often more prevalent in coastal areas and can vary in thickness and duration.
The portmanteau word for smoke and fog is "smog." This term is commonly used to describe a type of air pollution that combines fog with smoke or other pollutants, resulting in reduced visibility and harmful effects on health and the environment. Smog is often associated with urban areas where industrial activities and vehicle emissions are prevalent.
Fog can often develop in places that are near to bodies of water. They can also occur on flat-lying land and in valleys especially if the land is warmer than the air above it.
Fog is common along coastlines due to the interaction of warm, moist air from the ocean with cooler air over land. When the warm air rises and cools, it condenses into tiny water droplets, forming fog. Additionally, coastal areas often experience temperature differences between land and sea, which can enhance fog formation, especially in the early morning and late evening. This phenomenon is particularly prevalent in regions with upwelling currents that bring colder water to the surface.
Freezing fog, advection fog, and evaporation fog!
London fog : radiation fog enhanced by pollutants. Wisconsin fog : evaporation fog near water.
Pea soup fog is fog that is extremely thick, or heavy.
Ignorance is prevalent