Mist: Difference between revisions
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[[File:Kraftwerk im Dunst.jpg|thumb|250px|Power station visible through mist]] |
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[[File:Oberfallenberg 8.jpg|thumb|250px|Mist near the [[Austria]]-[[ Switzerland ]] border in December 2006.]] |
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'''Mist''' is a phenomenon caused by small droplets of [[water]] suspended in [[air]]. Physically, it is an example of a [[dispersion_(chemistry)|dispersion]]. It is most commonly seen where warm, moist air meets sudden cooling, such as in [[exhalation|exhale]]d air in the winter, or when throwing water onto the hot stove of a [[sauna]]. It can be created artificially with [[aerosol spray|aerosol canisters]] if the [[humidity]] and [[temperature]] conditions are right. It can also occur as part of natural [[weather]], when [[relative humidity|humid air]] cools rapidly, for example when the air comes into contact with surfaces that are much cooler than the air. |
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The formation of mist, as of other [[suspension_(chemistry)|suspension]]s, is greatly aided by the presence of [[nucleation site]]s on which the suspended water phase can congeal. Thus even such unusual sources as small particulates from [[volcanic eruption]]s, releases of [[hydrogen fluoride|strongly polar gas]]es, and even the [[magnetospheric]] ions associated with [[aurora|polar lights]] can in right conditions trigger the formation of mist. |
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==Description== |
==Description== |
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The only difference between mist and [[fog]] is visibility.<ref>http://www.rcn27.dial.pipex.com/cloudsrus/mistnfog.html</ref> The phenomenon is called fog if the visibility is one kilometre (1,100 yards) or less. In the UK the definition of fog is visibility less than 100 metres (for driving purposes, UK Highway Code rule 226),<ref>{{cite web|url=https://www.gov.uk/driving-adverse-weather-conditions-226-to-237/overview-226|title=Driving in adverse weather conditions (226 to 237)|work=www.gov.uk}}</ref> while for pilots the distance is one kilometre. Otherwise it is known as mist. |
The only difference between mist and [[fog]] is visibility.<ref>http://www.rcn27.dial.pipex.com/cloudsrus/mistnfog.html</ref> The phenomenon is called fog if the visibility is one kilometre (1,100 yards) or less. In the UK the definition of fog is visibility less than 100 metres (for driving purposes, UK Highway Code rule 226),<ref>{{cite web|url=https://www.gov.uk/driving-adverse-weather-conditions-226-to-237/overview-226|title=Driving in adverse weather conditions (226 to 237)|work=www.gov.uk}}</ref> while for pilots the distance is one kilometre. Otherwise it is known as mist. |
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Revision as of 14:38, 30 December 2017
 | This article needs additional citations for verification. (January 2009) |
Mist is a phenomenon caused by small droplets of water suspended in air. Physically, it is an example of a dispersion. It is most commonly seen where warm, moist air meets sudden cooling, such as in exhaled air in the winter, or when throwing water onto the hot stove of a sauna. It can be created artificially with aerosol canisters if the humidity and temperature conditions are right. It can also occur as part of natural weather, when humid air cools rapidly, for example when the air comes into contact with surfaces that are much cooler than the air.
The formation of mist, as of other suspensions, is greatly aided by the presence of nucleation sites on which the suspended water phase can congeal. Thus even such unusual sources as small particulates from volcanic eruptions, releases of strongly polar gases, and even the magnetospheric ions associated with polar lights can in right conditions trigger the formation of mist.
Description
The only difference between mist and fog is visibility.[1] The phenomenon is called fog if the visibility is one kilometre (1,100 yards) or less. In the UK the definition of fog is visibility less than 100 metres (for driving purposes, UK Highway Code rule 226),[2] while for pilots the distance is one kilometre. Otherwise it is known as mist.
Mist makes a beam of light visible from the side via refraction and reflection on the suspended water droplets.
"Scotch mist" is a light steady drizzle.
Mist usually occurs near the shores, and is often associated with fog. Mist can be as high as mountain tops when extreme temperatures are low.
Freezing mist
Freezing mist is similar to freezing fog, only the density is less and the visibility greater. (When fog falls below 0 degrees Celsius in temperature it is known as freezing fog.) [3]
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Mist lying in the folds of hills, Australia -
Sunlight through mist on a crisp winter morning -
Misty morning at Swifts Creek -
Mist on a lake -
Curitiba, Brazil
.jpg)
See also
References
- ^ http://www.rcn27.dial.pipex.com/cloudsrus/mistnfog.html
- ^ "Driving in adverse weather conditions (226 to 237)". www.gov.uk.
- ^ "WHAT IS DIFFERENCE BETWEEN ICE FOG AND FREEZING FOG?". theweatherprediction.com.