As air mass increases in temperature, its capacity to hold moisture also increases, which typically results in a higher dew point. The dew point is the temperature at which air becomes saturated with moisture and condensation begins to occur. Therefore, warmer air can contain more water vapor before reaching saturation, leading to a higher dew point in warmer conditions. Conversely, if the temperature decreases, the dew point will also decrease, indicating less moisture capacity.
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