What causes fog?
Autumn is known as the season of mists and mellow fruitfulness, but there was nothing mellow about the thick fog that blanketed much of the UK on Monday morning.
Visibility was widely reduced to less than 200m, with the worst affected areas seeing visibility as low as 50m for a time.
The fog has caused travel disruption – particularly for planes, with Heathrow Airport expected to cancel around 10 per cent of flights on Monday.
Poor driving conditions have reduced visibility, slowing traffic down, although it was still moving.
Fog is common in the UK during autumn, but what most people are surprised to hear is that there are four different types of fog, with radiation fog the type that affected us today.
What is the definition of fog?
The official definition of fog is when visibility is less than 1000m, which is often used with reference to aviation.
However, for the general public and motorists, thick fog is considered to be a visibility of 200m or less, with dense fog 50m or less – the point at which severe disruption to transport occurs.
How does fog form?
The mass of air over a particular location has its own characteristics, based on where its origins lie.
In autumn, air that arrives across the UK from the south west is warm and holds a lot of moisture.
When the air becomes saturated, it is no longer able to hold any more moisture, so the moisture condenses – producing tiny water droplets that become suspended in the air around us.
It is this abundance of tiny water droplets suspended in the air that reduces the visibility, forming fog. As you would imagine, the greater the number of water droplets, the lower the visibility and the denser the fog.
This type of fog occurs mainly during autumn, winter and early spring in the UK under clear skies. As the nights are longer, there is more time for temperatures to lower, as heat from the earth’s surface radiates back into space.
With a greater amount of cooling taking place, the chance that the dew point will be reached increases, with fog likely to form.
This type of fog occurs most often in winter and spring, when the land can be very cold and then warm, moist air from the Atlantic moves over it.
This is how sea fog forms and if the wind blows in the right direction, this sea fog and be blown on to the land – especially around coastal areas. This is also the cause of fog over snow when a thaw takes place.
This type of fog forms when warm, moist air is blown up the side of a hill or mountain.
As the temperature decreases with height, the warm, moist air is cooled as it travels further and further upwards.
The moisture in the air is eventually cooled enough to condense, forming hill fog – something that is hazardous for hill walkers or drivers travelling over higher routes.
This type of fog is caused by cold air passing over warmer water or moist land. In a way, it’s like an upside down version of advection fog.
As the cold air moves over the moist surface, some of the water evaporates into the air, which then cools and condenses, causing fog to form.
This type of fog is more common in autumn, when the sea is still warm from summer, yet has cold air moving over it from the east or north east.
In the simplest terms, fog is just a cloud on the ground – just as those fortunate enough to see the fog from above whilst travelling on a plane found out.
Flew into foggy London. Views are beautiful – this is the Shard and all the towers in the city pic.twitter.com/3j6AeF3Btt
— Sarah Wells (@sarahjwells) November 1, 2015
Fog is expected to return tonight for many areas, although by breakfast time tomorrow, it’ll probably mainly be across the Midlands, Northern England and southern Scotland.