Since warm air can hold more water vapor than cool air, raising or lowering temperature can change air's relative humidity (Figure to the right). The temperature at which air becomes saturated with water is called the air's dew point. This term makes sense, because water condenses from the air as dew if the air cools down overnight and reaches 100% humidity.

Clouds

Have you ever looked at the sky and found shapes in the clouds?Clouds have a great effect on the weather and climate, but they can also be lovely (if they're not pouring rain on you). It's fun to sit and watch the clouds go by.

Clouds and Relative Humidity

Air masses form over a large area; they can be 1,600 km (1,000 miles) across and several kilometers thick. Air masses form primarily in high pressure zones, most commonly in polar and tropical regions. Temperate zones are ordinarily too unstable for air masses to form. Instead, air masses move across temperate zones, so the middle latitudes are prone to having interesting weather.

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Air mass formation

What is the relationship between temperature and RH?

When temperature increases, relative humidity decreases