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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 8 · 25 questions

TOPIC PRACTICE

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  1. They provide condensation nuclei for water vapour
  2. They remove water vapour from air
  3. They turn fog into frost
  4. They always increase visibility
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  1. Cold moist air is trapped below and mixing decreases
  2. Warm air falls rapidly below
  3. Water vapour becomes stone
  4. Upper air pulls away all droplets
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  1. Dew (ओस)
  2. Frost (पाला)
  3. Mist (धुंध)
  4. Fog (कोहरा)
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  1. The relation of surface temperature to the freezing point (सतह के तापमान का हिमांक से संबंध)
  2. The speed of river flow (नदी की धारा की गति)
  3. The height of sea waves (समुद्री लहरों की ऊंचाई)
  4. The colour of rock (चट्टान का रंग)
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  1. Fog droplets remain suspended, whereas raindrops fall (कोहरे की बूंदें निलंबित रहती हैं, जबकि वर्षा की बूंदें गिरती हैं)
  2. Fog contains no water (कोहरे में जल नहीं होता)
  3. Rainfall is unrelated to water vapour (वर्षा जलवाष्प से असंबंधित है)
  4. Fog is always solid (कोहरा हमेशा ठोस होता है)
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  1. Scattering of light by tiny droplets (सूक्ष्म बूंदों द्वारा प्रकाश का प्रकीर्णन)
  2. Air weight becoming zero (हवा का भार शून्य हो जाना)
  3. Sunlight stopping completely (सूर्य का प्रकाश पूरी तरह बंद हो जाना)
  4. Water vapour becoming black (जलवाष्प का काला हो जाना)
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  1. Because their effects on visibility differ (क्योंकि दृश्यता पर उनका प्रभाव अलग होता है)
  2. Because mist contains no water (क्योंकि धुंध में जल नहीं होता)
  3. Because fog is always ice (क्योंकि कोहरा हमेशा बर्फ होता है)
  4. Because they form on different planets (क्योंकि वे अलग-अलग ग्रहों पर बनते हैं)
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  1. The open surface can undergo greater radiational cooling at night (खुली सतह रात में अधिक विकिरणीय शीतलन कर सकती है)
  2. An open field is always the sea (खुला मैदान हमेशा समुद्र होता है)
  3. An open field has no water vapour (खुले मैदान में जलवाष्प नहीं होती)
  4. An open surface blocks the Sun (खुली सतह सूर्य को रोकती है)
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  1. Because the availability of water vapour is low (क्योंकि जलवाष्प की उपलब्धता कम है)
  2. Because the surface does not cool on a clear night (क्योंकि साफ रात में सतह ठंडी नहीं होती)
  3. Because calm air always forms frost (क्योंकि शांत हवा हमेशा पाला बनाती है)
  4. Because dry air has no temperature (क्योंकि शुष्क हवा का कोई तापमान नहीं होता)
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  1. Because ice crystals can damage plant cells (क्योंकि बर्फ के क्रिस्टल पौधों की कोशिकाओं को नुकसान पहुंचा सकते हैं)
  2. Because dew contains no water (क्योंकि ओस में जल नहीं होता)
  3. Because frost is always hot (क्योंकि पाला हमेशा गर्म होता है)
  4. Because dew burns roots (क्योंकि ओस जड़ों को जला देती है)
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  1. Because only then water vapour can condense into tiny droplets (क्योंकि तभी जलवाष्प सूक्ष्म बूंदों में संघनित हो सकती है)
  2. Because air is completely dry at the dew point (क्योंकि ओसांक पर हवा पूरी तरह शुष्क होती है)
  3. Because the dew point is the temperature of a rock (क्योंकि ओसांक चट्टान का तापमान है)
  4. Because the dew point makes air pressure zero (क्योंकि ओसांक पर वायुदाब शून्य हो जाता है)
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  1. Evaporation of droplets due to solar heating (सौर ऊष्मा से बूंदों का वाष्पीकरण)
  2. Mist turning into stone (धुंध का पत्थर में बदलना)
  3. Water vapour becoming lava (जलवाष्प का लावा बन जाना)
  4. Complete absence of air (हवा का पूरी तरह अभाव)
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  1. They can provide tiny surfaces for droplet formation
  2. They completely remove water vapour
  3. They produce solar energy
  4. They turn air into stone
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  1. Surface cooling that keeps lower air cold
  2. Presence of water vapour
  3. Atmospheric air
  4. Existence of the Sun
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  1. When the surface reaches dew point by radiation
  2. When air has no water vapour
  3. When hot wind blows during day
  4. When surface becomes a sea wave
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  1. Normal liquid dew condition
  2. Cold condition related to frost or freezing deposit
  3. Hot wind
  4. Dry dust
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  1. Surface temperature above freezing and air dry
  2. Surface below freezing and air moist
  3. Clear cold night with enough moisture
  4. Night cooling in an open field
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  1. They are very tiny and remain suspended in air
  2. They are made of stone
  3. They remove gravity
  4. They stay only in the sea
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  1. The surface can fall below freezing because of stronger radiational cooling
  2. The surface always remains hot
  3. Water vapour completely disappears
  4. There is no air on a cloudless night
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  1. Dew formation may decrease
  2. Dew will always increase
  3. Frost will be compulsory
  4. Fog will always end
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  1. The air cools and approaches saturation
  2. Air pressure becomes zero
  3. Water vapour changes into soil
  4. Solar energy becomes infinite
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  1. The water supplies moisture and morning cooling encourages condensation
  2. Water bodies make the air completely dry
  3. Water bodies turn mist into frost
  4. There is no moisture in morning air
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  1. Tiny droplets scatter light and reduce visibility
  2. Fog changes sound into light
  3. There is no water in the air
  4. Fog erases the road
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  1. When the lower air becomes more saturated and droplet concentration increases
  2. When the air becomes completely dry
  3. When all droplets turn into stone
  4. When high temperature removes moisture
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  1. Because ice crystals can damage plant tissues
  2. Because dew always burns crops
  3. Because fog turns soil into stone
  4. Because frost instantly ripens crops

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