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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.

Medium · Level 9 · 25 questions

Practice questions

01When does the chance of dew-like moisture becoming frost increase?

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02Which statement correctly states both similarity and difference between mist and fog?

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03If fog seems to lift or clear after sunrise what is the reason?

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04Why can relative humidity be high near the surface during dew formation?

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05Why is low temperature alone not enough for frost formation?

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06Why can frost remain longer on shaded grass than on sunny open spots in a winter morning?

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07Why can dew on low grass and frost on a very cold nearby metal surface occur on the same night?

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08If the surface temperature is below dew point but above freezing point which condensation form is most likely to form?

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09If the surface is below freezing point and water vapour changes directly into ice crystals, what is this an example of?

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10Why can fog remain longer in a valley during the morning?

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11Which statement best explains the visibility-based difference between mist and fog?

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12Why is a clear and calm night especially favourable for dew formation?

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13Why may dew formation be less likely on a cloudy night?

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14How can strong wind weaken the process of dew formation?

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15If warm, moist air flows over cold land, what is the correct explanation for fog formation?

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16Why can steam-like mist form when cold air moves over a warm lake?

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17How can urban pollution particles help in dense fog formation?

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18Why can temperature inversion help fog persist?

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19Why can visual warning signals appear weak in dense fog?

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20Why can frost formation be more likely in an open field?

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21Why is frost considered more harmful to crops than dew?

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22Which is the correct location-based difference between dew and fog?

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23What is the correct importance of dust or smoke particles in fog formation?

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24If lower air is moist but the surface is warm, what condition will be lacking for fog formation?

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25Why can surface temperature sometimes be more important than air temperature in dew formation?

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