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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 10 · 25 questions

TOPIC PRACTICE

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  1. Condensation, then precipitation
  2. Floating, then an earthquake
  3. Melting, then evaporation
  4. Erosion, then deposition
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  1. Fog contains no water
  2. Raindrops remain permanently suspended in the air
  3. Fog is always made of ice
  4. Fog droplets are suspended in air, whereas raindrops fall
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  1. A warm, dry night with strong winds
  2. A surface below freezing with sufficient moisture in the air
  3. A cloudy, warm night
  4. A surface far above the dew point
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  1. Droplets can evaporate as the air near the ground warms
  2. The air turns to stone
  3. Water vapour disappears permanently
  4. The Sun becomes cold
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  1. The air is becoming completely dry
  2. The amount of suspended droplets is increasing and visibility is decreasing
  3. The surface is melting into lava
  4. Water vapour is being destroyed
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  1. They are exactly the same phenomenon.
  2. Frost forms or deposits on surfaces, whereas snowfall falls from clouds as precipitation.
  3. Frost forms only in the sea.
  4. Snowfall has no relation to atmospheric water vapour.
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  1. Dew has formed on a surface.
  2. Frost has formed on a surface.
  3. Tiny water droplets are suspended in the air.
  4. The soil contains no water.
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  1. All three may contain tiny water droplets or ice particles.
  2. All three form from rocks.
  3. All three contain no water vapour or condensed water.
  4. All three deposit only on land.
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  1. Evaporation
  2. Earthquake
  3. Salinity
  4. Weathering
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  1. Dew or frost
  2. Fog or mist
  3. Only snowfall
  4. Only frost
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  1. Dew
  2. Frost
  3. Fog
  4. Mist
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  1. Dew
  2. Frost
  3. Fog
  4. Mist
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  1. Dense fog
  2. Frost
  3. Mist
  4. Hail
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  1. Tiny droplets scatter light
  2. Oxygen disappears from the atmosphere
  3. Air turns black
  4. Ground suddenly rises
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  1. Frost forms by deposition on surfaces, snowfall falls from clouds
  2. Frost always falls with rain
  3. Snowfall forms only on grass
  4. There is no difference between them
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  1. Because droplets freeze into frost
  2. Because solar heat evaporates the droplets
  3. Because gravity disappears in air
  4. Because dew chemically changes into soil
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  1. Cold grass and leaves
  2. Hot sandy plain
  3. Sunlit wall at noon
  4. Warm seawater
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  1. White ice crystals appear on the surface
  2. Only dust moves in the air
  3. Visibility decreases only at sea
  4. Warm water flows on the surface
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  1. Both are completely identical
  2. Frost deposits on surface while snowfall falls from clouds
  3. Frost forms below sea floor
  4. Snowfall is unrelated to water vapour
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  1. Air becoming stone
  2. Permanent disappearance of water vapour
  3. Lower air warms and evaporates droplets
  4. Sun becoming cold
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  1. Presence of tiny droplets suspended in air
  2. Frost on surface
  3. Dew on surface
  4. Salinity in soil
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  1. Surface above freezing and near dew point
  2. Surface hot and dry
  3. Surface temperature below freezing and moisture available
  4. Strong noon sunshine
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  1. All three may contain condensed tiny water droplets or ice particles
  2. All three form from rocks
  3. All three are vapour-free
  4. All three deposit only on surfaces
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  1. Frost continually forms in the shade
  2. The shaded area receives less solar heat, so the ice crystals melt more slowly
  3. Sunlight turns frost into stone
  4. Water vapour is absent in the shade
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  1. Frost and snowfall
  2. Rain and frost
  3. Dew and mist
  4. Salinity and hot wind

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