Why can fog cause delays in air and road transport?
Fog makes it difficult to see distant objects clearly. Exam tip: remember fog with transport risk.
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Fog makes it difficult to see distant objects clearly. Exam tip: remember fog with transport risk.
View question detailsClouds reduce heat loss from the surface so it less often reaches dew point. Exam tip: consider clear nights favourable for dew.
View question detailsFog is made of tiny water droplets in the lower air. Exam tip: understand fog as droplets in air.
View question detailsWhen dew point is reached water vapour can change into liquid droplets. Exam tip: treat surface cooling as a condition for dew.
View question detailsWater vapour is invisible but droplets are visible. Exam tip: understand the difference between vapour and droplet.
View question detailsFrost deposits on surfaces and snowfall falls from above. Exam tip: distinguish by location and formation process.
View question detailsMist is linked with tiny droplets formed by light condensation. Exam tip: write moisture and cooling together.
View question detailsBelow freezing point water vapour can deposit as ice crystals. Exam tip: use temperature to identify dew and frost.
View question detailsWater vapour can more easily change into droplets on tiny particles. Exam tip: write the role of condensation nuclei in fog.
View question detailsMore droplets can form when air is close to saturation. Exam tip: connect dense fog with high moisture and cooling.
View question detailsBoth form from water vapour although their final forms differ. Exam tip: treat moisture as the basic condition.
View question detailsNight cooling can bring moist lower air to dew point. Exam tip: connect morning fog with cooling.
View question detailsMist is lighter than fog so visibility remains relatively higher. Exam tip: remember the visibility criterion.
View question detailsLiquid droplets identify dew while frost is ice crystals. Exam tip: choose the correct form by observing state.
View question detailsOn cooling moist air can approach saturation and form droplets. Exam tip: treat cooling as a basic condition for fog.
View question detailsFrost can appear as a white icy layer on cold open surfaces. Exam tip: treat cold open ground as a frost surface.
View question detailsFog and mist are made of tiny droplets floating in air. Exam tip: keep condensation and precipitation separate.
View question detailsGrass can cool quickly at night and reach dew point. Exam tip: take cold grass as a common example of dew.
View question detailsPollution particles can act as condensation nuclei and moist cool air can form fog. Exam tip: connect urban fog with particles and moisture.
View question detailsCooling of the surface can condense nearby moist air. Exam tip: take surface cooling as the main sign.
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