Do you sometimes feel much warmer than the actual observed temperature? ‘It’s not the heat, it’s the humidity’, right? Well not always—at higher temperatures that oppressive, muggy feeling (and frizzy hair) can actually be more about dew point than humidity.
What is dew point?
Dew point is the temperature to which air must be cooled in order to produce condensation (dew). It represents how much moisture is in the air: the higher the dew point temperature, the greater the atmospheric moisture content.
Dew point is the temperature to which air must be cooled in order to produce condensation (dew). It represents how much moisture is in the air: the higher the dew point temperature, the greater the atmospheric moisture content.
What’s the difference between dew point and humidity?
They both measure moisture in the air, but dew point is related to the quantity of moisture, while relative humidity expresses how close the air is to saturation. Relative humidity is the amount of moisture as a percentage of the amount that air can hold—and warmer air can hold more moisture than cooler air. So, if the amount of moisture in the air stays the same but the temperature rises, the relative humidity falls. Conversely, if temperature falls, relative humidity rises.
Because of its direct relationship to fluctuating temperature, relative humidity doesn’t provide suitable guidance on how much moisture is available at a specific location. Dew point however, is relatively consistent—unless affected by weather systems, such as troughs and fronts. For this reason, meteorologists prefer to use dew point when analysing atmospheric moisture and inferring what the conditions may feel like—represented by the apparent (‘feels like’) temperature.
They both measure moisture in the air, but dew point is related to the quantity of moisture, while relative humidity expresses how close the air is to saturation. Relative humidity is the amount of moisture as a percentage of the amount that air can hold—and warmer air can hold more moisture than cooler air. So, if the amount of moisture in the air stays the same but the temperature rises, the relative humidity falls. Conversely, if temperature falls, relative humidity rises.
Because of its direct relationship to fluctuating temperature, relative humidity doesn’t provide suitable guidance on how much moisture is available at a specific location. Dew point however, is relatively consistent—unless affected by weather systems, such as troughs and fronts. For this reason, meteorologists prefer to use dew point when analysing atmospheric moisture and inferring what the conditions may feel like—represented by the apparent (‘feels like’) temperature.
How does dew point affect the temperature you feel?
In warm, sultry weather, moisture in the air can impede your body’s ability to cool down. One of the ways your body cools itself is by the evaporation of moisture from your skin. When the air is moist, this process slows down—and you feel hotter for longer. So the higher the dew point, the longer it takes for your body to cool itself.
How you experience dew point varies, depending on your metabolism and the conditions you’re accustomed to, but it is possible to create an index of how an average person may feel at a certain dew point. This one uses Brisbane’s climate as an example.
In warm, sultry weather, moisture in the air can impede your body’s ability to cool down. One of the ways your body cools itself is by the evaporation of moisture from your skin. When the air is moist, this process slows down—and you feel hotter for longer. So the higher the dew point, the longer it takes for your body to cool itself.
How you experience dew point varies, depending on your metabolism and the conditions you’re accustomed to, but it is possible to create an index of how an average person may feel at a certain dew point. This one uses Brisbane’s climate as an example.
If you’re used to the tropics, you may find the ranges in this scale low—particularly during spring and summer where dew points are commonly above 24 °C. On the other hand, if you’re from southern Australia, you might find these ranges high.
So that old adage might better run, ‘It’s not the heat, it’s the moisture in the air, which at higher temperatures is more reliably indicated by dew point than humidity’. Think it will catch on?