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Subjects

Geography

Forms of condensation: dew, frost, fog, and mist

This Class 12 Geography topic from “Water in the Atmosphere” explains how water vapour changes into visible forms near Earth’s surface. Students learn how cooling, the dew point, relative humidity, and the availability of condensation nuclei produce dew, frost, fog, and mist. The topic distinguishes these forms by temperature, physical state, visibility, and formation conditions, including the role of surface cooling, calm air, and suspended droplets or ice crystals. It also helps students understand their effects on weather, visibility, agriculture, and daily life.

Easy · Level 2 · 25 questions

Practice questions

01What should the surface temperature generally be for frost to form?

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02Where does fog form?

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03Shining droplets on grass in the morning are an example of what?

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04How is frost different from dew?

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05Why does fog reduce visibility?

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06Why does a clear, calm night help dew form?

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07What is the change of water vapour into liquid water droplets on a cold surface called?

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08Why can a car window look misty on a cold morning?

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09In which season is frost generally seen more often?

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10What is necessary in air for fog formation?

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11When is dew generally seen more often?

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12Why is mist considered lighter than fog?

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13For dew formation, the surface temperature should be near what?

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14Why can fog be called a cloud near the ground?

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15Why can frost damage crops in fields?

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16What must be available in air for dew formation?

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17Why can very strong wind reduce dew formation?

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18Why does driving on roads become difficult in fog?

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19Which form can be made when water vapour directly changes into ice crystals?

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20How does air appear in mist?

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21What is the similarity between dew and frost?

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22Which condition is more favourable for fog?

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23Why may mist be more visible near a river or lake in the morning?

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24Fog and mist are both related to which process?

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25A white icy layer on leaves after a cold night may indicate what?

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