Question

When water particles condense on air and dust, it forms
A.Vapour
B.Fog
C.Mist
D.Frost

Answer 1

Hint: It is a phenomenon brought about by little beads of water suspended all around in the air. Genuinely, it is an illustration of a dispersion.

Complete answer: Mist is most ordinarily observed where warm, sodden air meets abrupt cooling, for example, in breathed out air in the colder time of year, or when tossing water onto the hot oven of a sauna. It tends to be made falsely with airborne canisters if the moistness and temperature conditions are correct. It can likewise happen as a feature of common climate, when muggy air cools quickly, for instance when the air comes into contact with surfaces that are a lot cooler than the air.
The formation of mist, as of different suspensions, is significantly helped by the presence of nucleation sites on which the suspended water stage can solidify. In this manner even such unusual sources as little particulates from volcanic ejections, arrivals of unequivocally polar gases, and even the magnetospheric particles related with polar lights can in right conditions trigger the development of mist. Mist is generally confused with fog, which looks like a stratus cloud lying at ground level. These two phenomena vary, yet share some regular things. Comparative cycles structure mist constantly. Fog is denser and by and large keeps going longer, yet the mist is more slender and more straightforward.

Thus, Option (C) is correct.

Note: Cloud cover is frequently alluded to as "mist" when experienced on mountains. Mist makes a light pillar obvious from the side through refraction and dissipating on the suspended water beads. Mist ordinarily happens close to the shores and is frequently connected with fog. Mist can be as high as peaks when extraordinary temperatures are low.