If high cirrus is followed by lower dense clouds how can weather change be explained?
High clouds followed by lower dense clouds can show development of a weather system. Exam tip: connect cloud sequence with weather change.
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High clouds followed by lower dense clouds can show development of a weather system. Exam tip: connect cloud sequence with weather change.
View question detailsDroplet growth in clouds and lower-air conditions determine surface rainfall. Exam tip: look at the whole atmospheric column.
View question detailsIn mixed clouds growing ice crystals can become precipitation particles. Exam tip: connect ice crystal growth with precipitation process.
View question detailsRain needs droplets to become sufficiently large and heavy. Exam tip: check both droplet number and droplet size.
View question detailsDescending warm air becomes more unsaturated and creates rain shadow. Exam tip: connect descending air with dryness.
View question detailsUpdrafts keep hailstones inside the cloud and ice layers grow on them. Exam tip: connect hail with uplift.
View question detailsA slow broad frontal system can maintain uplift and rainfall. Exam tip: observe speed and extent of the front.
View question detailsVertical temperature layers can change the final precipitation form. Exam tip: read lower warm and cold layers together.
View question detailsCondensation nuclei provide surfaces for droplet formation. Exam tip: connect scarcity of particles with cloud droplet formation.
View question detailsLonger residence in cloud can add water or ice layers to particles. Exam tip: understand the effect of updrafts.
View question detailsDrizzle has very fine droplets and light fall. Exam tip: notice differences within liquid precipitation.
View question detailsChanging cloud sequence can indicate development of a weather system. Exam tip: connect cloud sequence with weather change.
View question detailsMoisture is needed along with uplift for condensation and rain. Exam tip: check both moisture and uplift in orographic rain.
View question detailsTemperature decrease with height can keep ice crystals above and liquid droplets below. Exam tip: read vertical cloud structure.
View question detailsCollision and coalescence grow droplets to fallable size. Exam tip: identify the process of droplet growth.
View question detailsAn anvil-like top can be linked with a tall storm cloud. Exam tip: identify vertical growth and storm signs.
View question detailsDarkness of cloud is not a rainfall guarantee because lower-air conditions matter. Exam tip: examine the whole air column for surface rainfall.
View question detailsAt a front warm air rises cools and may form a cloud band. Exam tip: remember frontal uplift.
View question detailsStrong updrafts and cold zones help layer growth in hailstones. Exam tip: check both conditions for hailstorm.
View question detailsCloud type and uplift nature change rainfall extent. Exam tip: match rainfall style with cloud type.
View question detailsQUIZ COMPLETE