Why the dew point is a better measure of summer comfort than humidity

Why the dew point is a better measure of summer comfort than humidity
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In short: While relative humidity tells you how close air is to saturation, the dew point reveals the actual moisture content. When the dew point hits 20 °C, most people feel sticky. It is the most reliable predictor for cooling energy needs and a key factor in how effectively your body sheds heat.

The dew point is the temperature to which air must be cooled at constant pressure to reach 100% relative humidity. It is a thermodynamic property determined by the amount of water vapor present. When air temperature drops to the dew point, moisture capacity decreases, causing water vapor to condense into liquid. If this happens on a surface, it forms dew; if it happens in the air, it creates fog or clouds. When temperatures fall below freezing, this process is known as the frost point.

This metric is vital for understanding human comfort. Our bodies rely on the evaporation of perspiration to cool down, a process hindered by high moisture levels. In humid conditions, sweat cannot evaporate efficiently, leaving the skin coated and causing discomfort. While inhabitants of tropical climates may acclimatize to higher dew points, those in temperate regions often find levels above 15 °C uncomfortable, with 21 °C frequently described as oppressive. Conversely, extremely low dew points below −5 °C can cause skin irritation and dry out airways.

Beyond personal comfort, the dew point is a critical tool for aviation and meteorology. Pilots use it to estimate the base height of cumuliform clouds and to assess the risk of carburetor icing. Because the dew point is affected by barometric pressure, it varies with elevation; for instance, at the same temperature and dew point, air in Denver contains more water vapor than in New York City due to lower pressure at higher altitudes. Measuring it requires specialized devices like dew point meters, which use cooled mirrors to detect the onset of condensation.

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