What is the difference between mist, fog and haze?
Fog, mist and haze all affect visibility, which is an important part of forecasts affecting many aspects of life from driving conditions to shipping and aviation.
Fog and mist differ by how far you can see through it – fog is when you can see less than 1,000 meters away, and if you can see further than 1,000 metres we call it 'mist'.
In our meteorological glossary fog is defined as 'obscurity in the surface layers of the atmosphere, which is caused by a suspension of water droplets'.
By international agreement (particularly for aviation purposes) fog is the name given to resulting visibility less than 1 km, however in forecasts for the public this generally refers to visibility less than 180 m.
Mist is defined as 'when there is such obscurity and the associated visibility is equal to or exceeds 1000 m'. Like fog, mist is still the result of the suspension of water droplets, but simply at a lower density.
Mist typically is quicker to dissipate and can rapidly disappear with even slight winds, it's also what you see when you can see your breath on a cold day.
A third term you might also hear mentioned is haze. This is a slightly different phenomenon which is a suspension of extremely small, dry particles in the air (not water droplets) which are invisible to the naked eye, but sufficient to give the air an opalescent appearance.
These particles can also contribute to creating a red sky at sunrise or sunset.