Examples and humiditi of role of atmosphere
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For example, in the range of normal temperatures, air at 68 °F or 20 °C and 50 % relative humidity will become saturated if cooled to 50 °F or 10 °C, its dew point, and 41 °F or 5 °C air at 80 % relative humidity warmed to 68 °F or 20 °C will have a relative humidity of only 29 % and feel dry.
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