The altitude at which air is cooled to its dew point temperature and condensation begins is referred to as the lifting condensation level.

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This statement is true. The lifting condensation level (LCL) is the altitude at which air reaches its dew point temperature and becomes saturated, leading to the formation of clouds or precipitation. It is an important concept in meteorology and cloud formation.

The Altitude at Which Air Is Cooled to Its Dew