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Due to a phenononon called the Dry Adiabatic Lapse Rate. Air at the higher altitudes of a mountain summit will expend due to lower atmospheric pressures. As air expands, it cools at a rate of 9.8 degrees Celsius for every 1000m risen above sea level.

Therefore, on the summit of Mt Snowdon, UK, 1024m high, you could expect the temperature to be around 10 degrees cooler than it would be at sea level at any given time.

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