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Alto Cumulus Castellatus:
Definition of Alto Cumulus Castellatus: The term "Alto Cumulus Castellatus" refers to a type of cloud that forms when the Earth's atmosphere is perturbed by disturbances like thunderstorms, lightning, or even hurricanes. In its most classic form, these clouds are formed when there is an accumulation of warm air above a cold ground surface. The cumulus (the large clusters of clouds) are typically bright and white, as they are composed mostly of water droplets, which help them to persist in the atmosphere for hours. Example Sentence: "Did you know that Alto Cumulus Castellatus is actually a type of cloud formation when thunderstorms occur? It's a little eerie how these clouds can become so vibrant and colorful – like they're playing a hauntingly beautiful game with the sky!"
