The daily sequence of fog formation and later clearing is related to what?
Night cooling can form fog and daytime heat can evaporate droplets. Exam tip: remember the daily temperature cycle.
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SubjectsGeography
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Night cooling can form fog and daytime heat can evaporate droplets. Exam tip: remember the daily temperature cycle.
View question detailsWater vapour is an invisible gas while mist is visible due to condensed droplets. Exam tip: keep vapour and droplets separate.
View question detailsBecause of tiny size droplets can float in air. Exam tip: connect suspended droplets with fog and mist.
View question detailsDew forms at night and may evaporate by solar heat. Exam tip: identify the daily process sequence.
View question detailsFog is a form of suspended droplets in air near the surface. Exam tip: connect the lower air clue with fog.
View question detailsHeat loss is greater on a cloudless night and the surface can become very cold. Exam tip: connect clear sky with frost.
View question detailsStable moist air near the surface favours dew. Exam tip: understand the importance of a near-surface stable layer.
View question detailsWater vapour is invisible gas but condensed droplets are visible. Exam tip: remember the difference between vapour and droplets.
View question detailsWater surface supplies moisture and condensation can occur in cold morning. Exam tip: write moisture source and cooling together.
View question detailsWith less heat frost can remain solid longer. Exam tip: understand the effect of microclimate.
View question detailsSurface-specific cooling can change the form of condensation. Exam tip: treat surface temperature as decisive.
View question detailsWhen droplet number or density increases visibility decreases more. Exam tip: understand mist to fog through visibility change.
View question detailsIn rainfall drops fall toward the ground while fog and mist stay in air. Exam tip: separate precipitation and condensation.
View question detailsFrost needs moisture along with a cold surface. Exam tip: write temperature plus moisture in frost conditions.
View question detailsFrost can damage tender parts of crops. Exam tip: remember the agricultural effect of frost.
View question detailsBelow freezing point water can turn into solid ice crystals. Exam tip: treat freezing surface as the decisive clue.
View question detailsSolar heat can warm lower air and evaporate fog droplets. Exam tip: connect fog clearing with heating.
View question detailsCool surface air can approach saturation with the same moisture. Exam tip: remember the link between surface cooling and high humidity.
View question detailsMist is tiny droplets in air while frost is ice crystals on surfaces. Exam tip: observe the difference between air and surface.
View question detailsDew is surface liquid droplet frost is surface ice crystal and fog is air droplet. Exam tip: use both location and state for identification.
View question detailsQUIZ COMPLETE