If warm air slowly rises over cold air which rainfall is more likely?
Warm air rising over cold air is linked with frontal rainfall. Exam tip: observe meeting of air masses.
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Warm air rising over cold air is linked with frontal rainfall. Exam tip: observe meeting of air masses.
View question detailsTiny droplets and weak coalescence hinder precipitation formation. Exam tip: identify droplet growth conditions.
View question detailsDryness and weak precipitation process can reduce surface rain in rain shadow. Exam tip: separate cloud presence and rain amount.
View question detailsSupercooled droplets can freeze on hailstones and increase their size. Exam tip: remember layer growth of hail.
View question detailsLower thermal layers change the state of falling water. Exam tip: read lower layers for precipitation type.
View question detailsCloud colour alone does not decide rainfall intensity. Exam tip: check structure and motion along with colour.
View question detailsIn turbulent clouds droplets can collide and grow or break up. Exam tip: understand microprocesses in a balanced way.
View question detailsMoisture and continuous uplift give particles chance to grow. Exam tip: connect moisture plus uplift with precipitation.
View question detailsVertical development can make rainfall more local and intense. Exam tip: match cloud form change with rainfall style.
View question detailsFalling water from cloud may not fully reach the surface. Exam tip: understand difference between surface rain and aloft precipitation.
View question detailsCloud formation and precipitation are connected but separate stages. Exam tip: understand sequential but distinct processes.
View question detailsPrecipitation reaches the ground better when several conditions work together. Exam tip: examine the whole atmospheric column.
View question detailsLonger residence in cloud can let droplets grow by collision and freezing. Exam tip: connect updrafts with intense precipitation.
View question detailsLeeward air warms while descending and becomes relatively dry. Exam tip: understand rain shadow through descending warm air.
View question detailsDry lower air can evaporate falling drops before they reach the surface. Exam tip: remember virga-like conditions.
View question detailsIn mixed clouds ice crystal growth can strengthen precipitation. Exam tip: understand the importance of mixed phase clouds.
View question detailsMoisture distributed over many nuclei can increase droplet number but keep size small. Exam tip: study nuclei number and droplet size together.
View question detailsWhen different air masses meet warm air rises and cools. Exam tip: connect frontal lifting with cyclonic rain.
View question detailsAn anvil-like top is often linked with a tall developed storm cloud. Exam tip: treat anvil top as a cumulonimbus clue.
View question detailsWarm lower air can melt ice crystals into raindrops. Exam tip: check the vertical temperature profile.
View question detailsQUIZ COMPLETE