Overview
Relative humidity is a measure of the amount of moisture in the air relative to the total amount of moisture that the air can hold. For instance, if the relative humidity is 50%, then the air is half saturated with moisture.
Influencing Factors
Relative humidity is influenced by temperature and geographic location. Warmer air can hold more moisture than cooler air and warmer weather also promotes evaporation. Areas with a lot of surface water, such as coastal areas and the Great Lakes region, have high humidity levels due to evaporation. Humidity is especially high in warm, tropical areas.
Importance
Without humidity, there would be no fog, no clouds, and no precipitation. Humidity is simply water vapor in the air, which is needed to form rain. Additionally, water vapor holds heat in the air. It acts like a greenhouse gas, which means that it absorbs heat and warms the atmosphere. This is why humid air feels warmer.
Measurement
A capacitative sensor is used to measure relative humidity. Changes in relative humidity cause the shape of the sensor to change. When the sensor changes shape, its capacitance, or ability to store an electrical charge, changes in a detectable and repeatable fashion.