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Subjects

Geography

Humidity, evaporation, and condensation

This Class 12 Geography topic from “Water in the Atmosphere” explains how water moves between Earth’s surface and the atmosphere. Students learn to distinguish absolute and relative humidity, understand the factors that control evaporation, and examine how cooling causes condensation. The topic also connects these processes with dew, frost, fog, clouds, and precipitation, helping students interpret atmospheric moisture and its role in weather and climate.

Expert · Level 1 · 12 questions

Practice questions

01If energy is limited in evaporation, why can the rate remain limited even with a large humidity deficit?

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Answer and explanation

02Why can droplets remain very small even when condensation nuclei are abundant?

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03Why can atmospheric instability increase when moist air rises?

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04If saturation vapour pressure (e_s) increases much faster than actual vapour pressure (e), what generally happens to relative humidity (RH)?

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05Why can evaporation slow down after it increases the moisture in near-surface air?

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06Why can warm, humid air make the body feel hotter?

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07Why can pollution and fog persist together during a temperature inversion?

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08If both air temperature and dew point are rising, which conclusion is most reasonable?

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09Why can changes in atmospheric water vapour strongly affect local climate?

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10In which situation does coalescence help in rainfall formation?

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11If relative humidity (RH) rises from 40% to 80% while temperature stays the same, what does this mean?

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12Why can the night-time minimum temperature remain relatively higher when the air contains more moisture?

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Answer and explanation

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