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Cloud Development

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This overview outlines the essential steps in cloud development, starting with condensation and the role of salt particles as hygroscopic nuclei that attract water. It explains the mechanisms behind rising air motion that leads to cooling and saturation, and distinguishes between warm rain and cold cloud processes, including the phenomena of supercooled water and freezing rain. The text also highlights specific instances of freezing rain in the Northwest, such as in The Passes and Columbia Gorge, and discusses the implications of contrails on climate change.

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Cloud Development

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