Aerial view of a cumulonimbus storm cloud
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Aerial view of a cumulonimbus storm cloud
Cumulonimbus cloud. Aerial view of the anvil- shaped top, or thunderhead, of a cumulonimbus storm cloud. The thunderhead forms at the temperature inversion layer in the atmosphere, where the air above is warmer than the air below. The rising columns of moist, warm air which create cumulonimbus clouds are trapped by the inversion layer and so spread outwards. Cumulonimbus clouds can be up to 15 km tall and appear dark from beneath. The interior of a cumulonimbus cloud is highly turbulent, the built-up energy and water being released in the form of lightning and torrential rain or hail
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Media ID 6375975
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Aerial Aerial View Anvil Climate Cloud Cloud Types Clouds Cumulo Nimbus Meteorology Panoramic Storm Storm Cloud Thunderhead Type Weather Cumulonimbus Cloud
EDITORS COMMENTS
This aerial view showcases the majestic power of a cumulonimbus storm cloud. The anvil-shaped top, known as the thunderhead, dominates the image and reveals the immense height these clouds can reach - up to 15 km tall. Forming at the temperature inversion layer in the atmosphere, where warm air sits above cooler air, these towering columns of moist, warm air are trapped by this layer and spread outwards. From beneath, cumulonimbus clouds appear dark and ominous due to their density. However, it is within their turbulent interior that nature's fury truly comes alive. Built-up energy and water are released in spectacular displays of lightning and torrential rain or hail. This breathtaking photograph not only captures a remarkable moment in meteorology but also serves as a reminder of our planet's dynamic climate system. It highlights how different cloud types play crucial roles in shaping weather patterns and influencing our environment. The Science Photo Library has once again provided us with an awe-inspiring visual representation of nature's wonders. This print invites viewers to marvel at the raw power contained within this particular cumulonimbus cloud while appreciating its significance in understanding atmospheric phenomena.
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