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canvas prints spring canvas prints airplane canvas prints aircraft canvas prints atmospheric phenomenon canvas prints atmospheric physics canvas prints bird's eye view canvas prints cumulus cloud canvas prints cumulus humilis canvas prints european canvas prints french canvas prints low altitude canvas prints meteorological canvas prints no-one canvas prints nobody canvas prints plane canvas prints

photographs spring photos airplane photos aircraft photos atmospheric phenomenon photos atmospheric physics photos bird's eye view photos cumulus cloud photos cumulus humilis photos european photos french photos low altitude photos meteorological photos no-one photos nobody photos plane photos

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Cumulus humilis clouds seen from an aircraft over central France. Cumulus clouds typically occur under 2000 metres altitude. They form from water vapour in rising columns of air which condenses as it cools. Cumulus clouds often form at cold fronts where the advancing, cool air forces warm air upwards. The humilis variety occurs either as the first stage of the formation of other cumulus types, or when heat transfer (convection) in the atmosphere is weak. Due to its shallow depth, cumulus humilis does not produce any significant weather. These clouds, of a type known as cumulus humilis radiatus, have formed rows called 'streets'. Photographed in spring.

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