How do relative humidity and the dew point in an unsaturated air mass change with temperature variations?

In an unsaturated air mass, when the temperature increases, the capacity of the air to hold water vapor also increases. This means that for any given amount of moisture present in the air, an increase in temperature will result in a decrease in relative humidity. Relative humidity is defined as the ratio of the current amount of water vapor in the air to the maximum amount that the air can hold at a given temperature, expressed as a percentage. As temperature rises, while the actual moisture content remains the same, the relative humidity declines because the air can now hold more water vapor.

Moreover, the dew point, which is the temperature at which air becomes saturated with moisture and dew begins to form, remains constant unless actual moisture content changes. Since we are considering a scenario where the moisture content does not change, the dew point remains stable despite the increase in ambient temperature.

This understanding emphasizes the relationship between temperature, relative humidity, and dew point, highlighting the impact of temperature on the ability of air to contain moisture without necessarily altering the actual moisture content.