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Similar to other clouds, contrails can cast shadows, in that an aircraft and its contrail are actually high up in the sky, while the shadow is cast downwards onto the cirrus haze layer by the sun or the moon. The thin layer acts as a canvas upon which the shadow is projected. In the end, contrail shadows are a captivating atmospheric optical phenomena that sometimes appears counter-intuitive. This example of such a contrail and its shadow was spotted over Columbus, Ohio, US.

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Cumulus homogenitus, which is cloud development as a result of human activity, such as the steam rising from the boiler roof stacks on top of buildings on the Upper West Side, Manhattan, New York, US.

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Cirrus homogenitus as a result of aircraft condensation trails, also known as contrails, in the upper atmosphere. When these types of clouds persist and evolve towards a more natural appearance, its cloud classification changes from homogenitus to homomutatus. This example was spotted over Abergavenny, Wales.

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