Do You Know The Best Way To Tell How Moist The Air Is? Believe It Or Not, "Humidity" Isn’t The Answer

Why You Should Care About The Dew Point

There are multiple ways to describe how wet the air is (yes, pretty much all air is wet). What I mean by that is there are water molecules tucked in between the gases like nitrogen and oxygen that make up the air around us.

How much water is in the air is important to human comfort and safety, largely because it impacts your body’s natural cooling system: sweat.

But not all methods of communicating how moist the air is are created equal.

The two most commonly used measurements are the relative humidity and the dew point.

While you may be more used to hearing about the relative humidity, the dew point is actually a much more useful number.

That is because the dew point is a measure of how much water vapor is in the air and relative humidity is a measure of how much water vapor is in the air relative to how much water vapor could be in the air.

That sentence was pretty long and hard to follow, so let’s break it down.

Dew point is an absolute measure of moisture content in the air: A higher dew point directly means that there is more water vapor in the air. This matters for how comfortable the air is outside because it impacts your body’s ability to use sweat as a method of self-cooling.

Sweat cools your body through evaporation. When you sweat, small water droplets collect on your skin. As those droplets evaporate, they take energy from your body, cooling you, and from the air directly above your skin, keeping you more comfortable.

(MORE: The Good And The Bad About Sweat On The Skin)

Technically speaking, the dew point is the temperature at which air would be saturated (meaning it has a 100% relative humidity). When air is saturated, the water vapor condenses into droplets and you get features like clouds and fog.

Relative humidity is a relative measure of moisture content in the air: Relative humidity is a measure of how much moisture is in the air relative to how much there could be based on the temperature.

Warm air can hold more moisture than cold air, so as the temperature changes, the relative humidity does as well, even if the actual moisture content in the atmosphere isn’t changing.

This is a very common trend for daily relative humidity cycles. On a typical day (barring any fun weather phenomena like cold fronts and the like), temperatures go from cool in the morning to warm in the afternoon, then back to cool at night.

Relative humidity has an opposite trend (again, making an assumption that the moisture content in the atmosphere is changing very little or not at all). It starts high in the morning, drops in the afternoon and then rises again at night as things cool off.

Often, it will feel most humid during the afternoon when the relative humidity is the lowest.

When it comes to the physiological processes that keep you cool, knowing how much moisture is in the air is much more important than how much moisture the air could have.

Climate snapshot: High humidity on a hot day is more than just uncomfortable - it can be deadly. And days like that are increasing in frequency across the country.

Climate Central warns that high humid heat days more than doubled in frequency for most of the regions in the country from 1980 to 2020.

Sara Tonks is a content meteorologist with weather.com and has a bachelor’s and a master’s degree from Georgia Tech in Earth and Atmospheric Sciences along with a master’s degree from Unity Environmental University in Marine Science.