If mist gradually becomes denser, what may it appear to become?
As droplet concentration increases, visibility reduces more and the condition appears like fog. Exam tip: understand mist to fog through visibility.
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SubjectsGeography
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As droplet concentration increases, visibility reduces more and the condition appears like fog. Exam tip: understand mist to fog through visibility.
View question detailsDew, frost, fog, and mist are linked with transformation of atmospheric moisture. Exam tip: remember cooling and moisture as the common idea.
View question detailsNight cooling can bring moist air near the surface to the dew point. Exam tip: connect morning fog with surface cooling.
View question detailsDew forms when water vapour changes into liquid droplets on a cold surface. Exam tip: remember dew point with surface condensation.
View question detailsFrost forms as ice crystals so the surface must be very cold. Exam tip: distinguish dew and frost by state.
View question detailsBoth fog and mist consist of tiny water droplets suspended in the air, but they are mainly distinguished by the extent of reduced visibility. Fog is denser and reduces visibility much more than mist. Air pressure and colour are not the main criteria used to distinguish them. Exam tip: remember that fog is denser, so it causes poorer visibility.
View question detailsA clear night allows quick surface cooling and calm air keeps the moist layer. Exam tip: remember clear calm nights for dew.
View question detailsCold air can collect in valleys and come close to saturation. Exam tip: connect valleys with cold-air pooling.
View question detailsFrost forms when water vapour deposits in icy form. Exam tip: treat a white layer as a sign of frost.
View question detailsFog droplets scatter light and blur distant objects. Exam tip: write water droplets as the cause of low visibility.
View question detailsA water surface supplies moisture and morning cooling can cause condensation. Exam tip: see water source and cooling together.
View question detailsHeat from sunshine evaporates dew droplets. Exam tip: remember morning dew and daytime evaporation sequence.
View question detailsBoth dew and frost form from atmospheric water vapour. Exam tip: remember moisture as similarity and state as difference.
View question detailsFor dew the surface must cool to the dew point. Exam tip: do not treat moisture alone as sufficient.
View question detailsFog and mist both consist of tiny water droplets in air. Exam tip: treat both as condensation in air.
View question detailsA cold window can cool moist air to the dew point. Exam tip: identify condensation through daily life examples.
View question detailsCalm moist air near the surface is favourable for dew. Exam tip: treat strong wind as unfavourable for dew.
View question detailsVisibility in mist is not as low as in fog. Exam tip: remember the difference on the basis of visibility.
View question detailsWater deposited as liquid droplets on a surface is dew. Exam tip: keep the difference between liquid droplets and ice crystals.
View question detailsFrost forms when water vapour deposits as ice crystals. Exam tip: connect direct ice formation with frost.
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