Katabatic wind

A katabatic wind is a downslope wind caused by the flow of an elevated, high-density air mass into a lower-density air mass below. The spelling catabatic is also used. Since air density is strongly dependent on temperature, the high-density air mass is usually cooler, and the katabatic winds are relatively cool or cold.

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Source: Wikipedia · Image: Wikimedia Commons · CC BY-SA 4.0

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