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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.

Medium · Level 3 · 25 questions

TOPIC PRACTICE

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  1. Because air in valleys always remains hot
  2. Because valleys have no water vapour
  3. Because cold dense air can collect below and become saturated
  4. Because valleys double solar radiation
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  1. Convective storm
  2. Dust storm
  3. Mountain snowfall
  4. Advection fog
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  1. Because air near the surface can cool to dew point
  2. Because grass destroys water vapour
  3. Because grass always produces ice
  4. Because warm air prevents condensation
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  1. Because fog melts the road
  2. Because visibility decreases and drivers cannot see far
  3. Because fog makes vehicles lighter
  4. Because gravity disappears in air
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  1. Because mist contains only dust
  2. Because mist has no form of water
  3. Because droplet concentration is lower and visibility remains greater
  4. Because it always forms below the ground
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  1. It instantly turns plants into soil
  2. It completely stops rainfall
  3. It permanently blocks sunlight
  4. It can damage tender plant cells by forming ice crystals
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  1. Dew forms on surfaces and fog forms in air near the ground
  2. Dew forms only in sky and fog underground
  3. Dew forms in sea and fog inside mountains
  4. Both form only in plant roots
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  1. Snow crystal
  2. Dew
  3. Lava
  4. Dust storm
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  1. It turns droplets into stones
  2. It turns vapour into oxygen
  3. It warms air and increases evaporation of droplets
  4. It turns land into sea
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  1. Melting of glass
  2. Sun directly becoming water
  3. Air becoming completely dry
  4. Condensation of water vapour on a cold surface
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  1. Saturation
  2. Complete dryness
  3. Sea salinity
  4. Underground boiling
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  1. Because dry air lacks sufficient water vapour
  2. Because dry air always has a high dew point
  3. Because dry air raises the surface temperature and causes condensation
  4. Because dry air has no atmospheric pressure
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  1. Cold air pooling below and possibility of frost
  2. High sea waves
  3. Hot desert sand
  4. Earthquake intensity
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  1. Availability of water vapour
  2. Volcanic ash
  3. Sea tide
  4. Dry hot wind
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  1. Dust fog
  2. Mountain fog
  3. Evaporation fog
  4. Sandy fog
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  1. Because the air near the surface will not reach saturation
  2. Because water vapour will always change into ice crystals
  3. Because gravity does not act on a warm surface
  4. Because dew forms only over the sea
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  1. They remove water vapour
  2. They provide tiny bases for droplets
  3. They always keep air warm
  4. They immediately make visibility infinite
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  1. Moving directly underground
  2. Remaining completely still
  3. Falling as stone from above
  4. Moving horizontally over a cold surface
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  1. Because droplet concentration is lower in mist
  2. Because mist has no water
  3. Because mist is always hot lava
  4. Because mist is invisible only at night
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  1. Because frost is never ice
  2. Because frost can also form by vapour directly becoming ice
  3. Because frost forms only in the sea
  4. Because frost has no relation to water
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  1. Scattering of light by water droplets in air
  2. Shrinking size of the Sun
  3. Stopping of Earth's rotation
  4. Drying of the ocean
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  1. Because it becomes stone
  2. Because it can evaporate due to solar heating
  3. Because leaves eat it
  4. Because there is no water in air
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  1. Surface is below freezing
  2. Air has moisture
  3. Surface is warm and air is dry
  4. Night is long and cold
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  1. Weathering
  2. Meandering
  3. Condensation
  4. Tide
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  1. Because air near the surface can reach dew point
  2. Because air becomes completely dry
  3. Because water vapour ends
  4. Because ocean water increases

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