Mist is a weather phenomenon consisting of tiny water droplets suspended in the air. While it is often used interchangeably with fog, it is technically defined by : if you can see further than one kilometer (about 0.6 miles), it is classified as mist ; if you cannot, it is fog . Scientific Insights
: For mist to form, water vapor needs a "seed" to cling to. This can be microscopic dust, salt, pollen, or even volcanic ash. Mist is a weather phenomenon consisting of tiny
: In Scotland , this term refers to a specific combination of thick mist and very light, steady drizzle. This can be microscopic dust, salt, pollen, or
: When temperatures drop below freezing, these droplets remain liquid (supercooled) until they touch a surface, where they instantly turn into ice. Cultural & Mythological Significance What's the difference between mist and fog? - BBC Newsround Mist forms when warm
: Volcanologists study mist emitted from steam vents to predict eruptions. A sudden temperature rise of just a few degrees in the mist can signal an impending explosion.
Mist forms when warm, moist air is rapidly cooled, causing invisible water vapor to condense into liquid droplets.