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(the mountain diagram) 1) Fill in the blanks (temperatures in Celsius) of the mountain diagram and answer the questions below
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Answer #1

Altitude has no effect on the dew point of a parcel of air. It is the temperature to which a parcel must be cooled to saturate. So when the air parcel rises, its temperature changes, and when it reaches the dew point, it gets saturated and precipitates.

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