Why are dew, frost, fog, and mist kept under forms of condensation?
All these forms are produced by cooling of atmospheric moisture. Exam tip: remember the common idea as cooling and moisture.
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SubjectsGeography
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All these forms are produced by cooling of atmospheric moisture. Exam tip: remember the common idea as cooling and moisture.
View question detailsIn dense fog many tiny droplets scatter light. Exam tip: remember reduced visibility as the main effect of fog.
View question detailsWater vapour changes into liquid droplets on the cold glass. Exam tip: understand droplets on a cold surface as dew.
View question detailsDew forms when water vapour changes into liquid droplets on a cold surface. Exam tip: remember dew as droplets on a surface.
View question detailsFrost forms as ice crystals on a very cold surface. Exam tip: identify a white icy layer as frost.
View question detailsFog forms from tiny water droplets present in air near the ground. Exam tip: understand fog as a cloud near the surface.
View question detailsMist is lighter than fog and reduces visibility slightly. Exam tip: understand mist as lighter fog.
View question detailsDew needs a cold surface and moisture in air. Exam tip: remember the two conditions of dew together.
View question detailsFrost forms when the surface temperature is below freezing and water vapour changes directly into a solid. Therefore, water appears as ice crystals in frost. Dew is the closest distractor, but it consists of liquid water droplets. Exam tip: below-freezing temperatures favour frost rather than dew.
View question detailsTiny droplets in dense fog obstruct distant vision. Exam tip: write reduced visibility as the main effect of fog.
View question detailsBoth form from atmospheric water vapour but their states differ. Exam tip: remember moisture as similarity and state as difference.
View question detailsFog and mist form when water vapour condenses into tiny droplets. Exam tip: treat them as forms of condensation.
View question detailsLiquid droplets on leaves in the morning are a common example of dew. Exam tip: connect droplets on leaves with dew.
View question detailsOn a below-freezing surface water vapour may deposit as ice crystals. Exam tip: distinguish dew and frost by temperature.
View question detailsIn fog tiny droplets remain suspended in air. Exam tip: remember fog structure as droplets in air.
View question detailsDew point is the temperature at which air approaches saturation. Exam tip: connect dew point with dew formation.
View question detailsMist obstructs visibility less than fog. Exam tip: remember their difference by visibility.
View question detailsOn a clear night radiational cooling can cool the surface to dew point. Exam tip: remember the relation between clear night and dew.
View question detailsIn winter frost can form on very cold surfaces. Exam tip: connect winter and white deposit with frost.
View question detailsMoist air can become saturated on cooling and form fog. Exam tip: mention both moisture and cooling.
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