If a cloud has very strong vertical development why can sudden heavy rainfall occur?
Stormy vertical clouds can cause rapid droplet growth and heavy rain. Exam tip: connect vertical development with rain intensity.
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Stormy vertical clouds can cause rapid droplet growth and heavy rain. Exam tip: connect vertical development with rain intensity.
View question detailsDifferent parts of a cloud can have different temperatures so liquid and solid particles may coexist. Exam tip: understand mixed clouds.
View question detailsIn thin clouds fallable droplet growth may be limited. Exam tip: separate visible cloud from rain cloud.
View question detailsDust particles can help droplet formation as condensation nuclei. Exam tip: understand nuclei as tiny surfaces.
View question detailsA vertically growing cumulus can change into cumulonimbus. Exam tip: connect growing cumulus with storm potential.
View question detailsLayers below or above freezing level can decide rain snow or mixed forms. Exam tip: connect freezing level with precipitation type.
View question detailsWhen snowflakes pass through a relatively warm layer of air, they may melt only partly and reach the ground as a mixture of rain and snow. Hail forms through repeated freezing and growth in strong storm clouds, not simply by partial melting of snowflakes. Exam tip: use the temperature layers between the cloud and the ground to identify the type of precipitation.
View question detailsMoisture and mountain uplift together increase condensation and rain. Exam tip: see maritime moisture and orographic uplift together.
View question detailsLarge drops and wind can increase surface impact. Exam tip: understand physical effects of heavy rain.
View question detailsHeight and form identify types like cirrus stratus and cumulus. Exam tip: remember cloud classification criteria.
View question detailsCollision and coalescence can grow droplets and make them fall. Exam tip: connect coalescence with rain formation.
View question detailsDense clouds block more light so it can look dark below. Exam tip: connect cloud darkness with density.
View question detailsDrizzle is light precipitation of very small liquid droplets. Exam tip: connect drizzle with small liquid drops.
View question detailsA cold lower layer can keep ice particles solid. Exam tip: check lower air for precipitation type.
View question detailsLeeward descent makes air warm and dry. Exam tip: remember mountain crossing and leeward dryness.
View question detailsNimbostratus clouds are linked with long-lasting widespread rain. Exam tip: match cloud type with rainfall style.
View question detailsCondensation nuclei provide tiny surfaces for droplets. Exam tip: connect lack of nuclei with cloud droplet formation.
View question detailsClouds and precipitation are connected but not the same process. Exam tip: remember connected but distinct stages.
View question detailsRepeated uplift can freeze ice layers and form hail. Exam tip: connect repeated updrafts with hailstorm.
View question detailsEvaporation in lower air can reduce rain reaching the surface. Exam tip: understand cloud precipitation versus surface rainfall.
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