If a cloud is very dark but droplet growth is limited why will heavy rain not be certain?
Cloud darkness may show density but rainfall needs droplet growth. Exam tip: separate appearance from process.
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Cloud darkness may show density but rainfall needs droplet growth. Exam tip: separate appearance from process.
View question detailsLayered clouds can give widespread rain and vertically developed clouds local intense rain. Exam tip: match cloud type with rainfall style.
View question detailsCollision and coalescence help droplets become fallable. Exam tip: connect coalescence with rain formation.
View question detailsSupercooled droplets increase ice layers on hailstones. Exam tip: connect hail growth with supercooled droplets.
View question detailsA change in cloud sequence can indicate a developing weather system. Exam tip: connect cloud sequence with weather change.
View question detailsThe leeward area can receive low rainfall due to rain shadow. Exam tip: remember the relief and climate relation.
View question detailsLower temperature aloft can maintain ice crystals while liquid droplets remain below. Exam tip: connect cloud layers with temperature.
View question detailsLower thermal layers can change the state of falling water. Exam tip: check the full thermal profile for precipitation type.
View question detailsHumid air can become saturated at a lower height. Exam tip: understand relative humidity and cloud base relation.
View question detailsHeavy precipitation needs enough uplift and particle growth along with moisture. Exam tip: see moisture plus uplift together.
View question detailsIn virga precipitation falls from cloud but does not reach the surface. Exam tip: treat dry lower air as the main clue.
View question detailsTiny droplets do not reach fallable weight. Exam tip: identify droplet growth conditions.
View question detailsMoisture is necessary along with uplift. Exam tip: check both uplift and moisture for orographic rainfall.
View question detailsRepeated vertical motion can add icy layers to hailstones. Exam tip: connect hailstone growth with repeated updrafts.
View question detailsLarger droplets can fall rather than remain suspended. Exam tip: check droplet size along with water content.
View question detailsLower air can change both form and amount of precipitation. Exam tip: pay attention to the full air column.
View question detailsConvectional rainfall can be very intense over a small area. Exam tip: connect local intensity with convection.
View question detailsCold lower layers prevent ice crystals from melting. Exam tip: remember cold column for snow.
View question detailsMixed particles and strong vertical motion can enhance storm precipitation. Exam tip: remember cumulonimbus hazards.
View question detailsEvaporation in lower air can reduce rain reaching the surface. Exam tip: separate cloud precipitation and surface rainfall.
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