Fog near the ground and cloud at height are mainly distinguished on what basis?
Fog is a mass of tiny droplets near the ground while cloud is at height. Exam tip: use location as the main difference.
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Fog is a mass of tiny droplets near the ground while cloud is at height. Exam tip: use location as the main difference.
View question detailsA cold surface can cool moist air and cause condensation. Exam tip: link contact cooling with fog formation.
View question detailsEvaporation from warm water and condensation in cold air can form mist. Exam tip: identify the warm water and cold air combination.
View question detailsWater vapour can form tiny droplets on dust and smoke particles. Exam tip: write the role of particles in urban fog.
View question detailsIn inversion vertical mixing is weak and lower moist air remains trapped. Exam tip: connect inversion with fog trapping.
View question detailsWhite icy crystals are the identity of frost. Exam tip: treat liquid droplets as dew and ice crystals as frost.
View question detailsTheir location can be similar but their final state differs. Exam tip: use state as the main difference.
View question detailsFog is a form of condensation while rain is falling precipitation. Exam tip: keep condensation and precipitation separate.
View question detailsFog droplets scatter light and reduce viewing distance. Exam tip: connect visibility with droplet scattering.
View question detailsOpen surfaces can cool rapidly and fall below freezing. Exam tip: connect open cold surfaces with frost.
View question detailsDew needs enough moisture along with surface cooling. Exam tip: do not treat clear night alone as sufficient.
View question detailsFrost can form an icy layer on plants and damage tissues. Exam tip: connect frost damage with agriculture.
View question detailsAt dew point air approaches saturation and droplets can form. Exam tip: connect dew point with fog formation.
View question detailsAs temperature rises mist droplets can become water vapour again. Exam tip: understand morning mist and daytime heating.
View question detailsDew is droplets on a surface while fog is a mass of droplets in lower air. Exam tip: identify the form by location.
View question detailsThese particles can act as condensation nuclei. Exam tip: understand the role of tiny surfaces in droplet formation.
View question detailsFog needs cooling of lower air along with moisture. Exam tip: write moisture plus cooling together.
View question detailsFor dew the surface cooling to dew point can be decisive. Exam tip: separate surface temperature and air temperature.
View question detailsBoth form from atmospheric moisture but their final forms differ. Exam tip: remember moisture as similarity and state as difference.
View question detailsNear or below freezing point water can take solid form. Exam tip: connect freezing droplets with frost-like cold conditions.
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