If fog forms only over a river but not over nearby dry land what is the most appropriate reason?
A river is a moisture source and that moisture can condense in cool air. Exam tip: connect moisture source with fog formation.
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SubjectsGeography
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A river is a moisture source and that moisture can condense in cool air. Exam tip: connect moisture source with fog formation.
View question detailsSunlight can first melt frost into liquid water and then evaporate it. Exam tip: read the sequence of state changes carefully.
View question detailsMore tiny droplets scatter more light so visibility decreases. Exam tip: connect dense fog with low visibility.
View question detailsDew forms when moist air near the surface becomes saturated at the dew point. Exam tip: connect dew with surface condensation.
View question detailsFrost forms when water vapour changes into ice crystals on a freezing surface. Exam tip: distinguish dew and frost by surface temperature.
View question detailsFog reduces visibility more than mist. Exam tip: treat both as visibility phenomena made of tiny droplets.
View question detailsA clear sky cools the surface fast and calm air keeps moisture near it. Exam tip: link clear calm nights with dew.
View question detailsSurface condensation above freezing gives liquid droplets called dew. Exam tip: separate conditions above and below (0^\circ C).
View question detailsDirect change of vapour into ice is deposition and can form frost. Exam tip: connect frost with deposition.
View question detailsCold moist air may get trapped in valleys and vertical mixing decreases. Exam tip: remember valley fog with temperature inversion.
View question detailsAdvection fog forms when horizontally moving moist air cools over a cold surface. Exam tip: connect advection with horizontal movement.
View question detailsWarm water supplies moisture and cold air becomes saturated quickly to form fog. Exam tip: connect steam fog with warm water and cold air.
View question detailsDew is surface condensation and fog is like a cloud near the ground. Exam tip: distinguish them by location.
View question detailsCondensation does not start if the surface does not cool to the dew point. Exam tip: remember the dew point threshold.
View question detailsDust and smoke particles provide surfaces for water vapour condensation. Exam tip: call pollution particles condensation nuclei.
View question detailsInversion prevents vertical mixing, so fog disperses slowly. Exam tip: write inversion as a trapping condition.
View question detailsFog greatly reduces visibility near the ground through tiny droplets. Exam tip: identify fog by poor visibility.
View question detailsMist has tiny droplets but is not as dense as fog. Exam tip: connect mist with lighter visibility reduction.
View question detailsSunlight warms the surface and dew droplets can become vapour again. Exam tip: connect dew disappearance with evaporation.
View question detailsFrost is linked with freezing conditions and can damage crops. Exam tip: connect frost with crop damage.
View question detailsQUIZ COMPLETE