Relative humidity refers to the amount of moisture in the air compared to the maximum amount the air can hold. It is measured as a percentage using instruments like a psychrometer, which measures the temperature difference between a wet-bulb and dry-bulb thermometer, or a hair hygrometer, which uses the stretching of human or animal hair to gauge humidity over time. Absolute humidity refers to the actual amount of water vapor in the air regardless of temperature, while specific humidity is the weight of water vapor contained in a unit weight of air. High relative humidity occurs when air already contains most of the moisture it can hold, making it feel hotter, while low relative humidity means air can still hold more moisture and feels cooler.