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An iceberg can change to fog through a process called sublimation, where solid ice transitions directly to water vapor without becoming liquid. As an iceberg melts in warmer conditions, it releases moisture into the air, which can contribute to fog formation. Additionally, if the surrounding air is cooler than the surface temperature of the iceberg, the moisture can condense into tiny water droplets, creating fog. This process highlights the interplay between temperature, humidity, and phase changes in the atmosphere.

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1mo ago

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