How Can Condensation Occur at Higher Air Temperature?
Condensation happens when moist air meets something below the dew point temperature. Cool the grass overnight with lower air temperature and night-sky radiation, and dew forms in the morning—a drop in temperature causes the condensation. Simple enough. But here’s a condensation conundrum: you can raise the temperature and get condensation, too. That’s what happens inside an air compressor tank. Same physics, opposite direction. But how?
The magic of pressure
Moist air is a mixture of two components: (1) dry air (mostly nitrogen and oxygen) and (2) water vapor. The amount of water vapor determines the dew point temperature. More water vapor means higher dew point. When that moist air finds a material at the dew point or below, condensation is the result.
That’s the standard lesson on humidity and condensation. But there’s an assumption built into that lesson: that the pressure is constant (or close). You already know that pressure has another effect on water. Go high up into the mountains and boil some water, and your tea won’t be as hot. The lower air pressure of high elevations reduces the boiling point of water. Likewise, raising the air pressure increases the boiling point, which is why your food cooks more quickly in a pressure cooker.
What’s the connection here? Boiling point is the temperature where liquid water turns to vapor. Dew point is the temperature where water vapor turns to liquid. They’re two sides of the same coin, and pressure moves both of them the same direction: Raise the pressure, and you raise the temperature at which that phase change happens—for boiling and for condensing.
But I’m not talking about the small pressure swings that come with changes in the weather. Barometric pressure changes by a fraction of an inch of mercury from a passing front. That’s nowhere near enough to matter. I’m talking about multiplying the pressure several times over, the way a compressor takes air from 14.7 psi up to 100 psi or more.
Enter the compressor
If you’ve ever used a compressor for nail guns or inflating basketballs, you may have seen the effect of pressure on dew point temperature. The photo below shows what happens when you drain a compressor after using it. If you want your compressor to last, you have to open the valve at the bottom of the tank to drain the water that collected during use. That bit water on the concrete is from condensation inside the tank. And that was after I used the compressor for only a few minutes. Use it several hours or all day, and there will be considerably more.

That is the effect of pressure. Raise the pressure and the dew point temperature of water vapor increases, just as the boiling point temperature of water does.
And the fact that I’m talking about this happening in a compressor is important. Yes, you can get condensation when the outdoor temperature is 90 °F, but you won’t see that happening just because of changes in the weather. The air pressure inside a compressor tank is 5 to 10 times higher than atmospheric pressure.
Pressure in the psychrometric chart
If you’ve ever learned how to use the psychrometric chart, you know it’s a complex mess of lines and curves that can tell you how to find dew point if you know two other psychrometric variables. Usually you’d have air temperature (dry bulb) and relative humidity, but there are a bunch of other psychrometric variables, too.
Here’s the thing you may not have known, though. Or forgotten if you did. When you’re looking at a psychrometric chart, it was made for a specific pressure. If the pressure changes significantly, you need a new chart.
So there’s your answer: Dew forms from a temperature drop at normal pressure; compressor condensation forms from a temperature rise at much higher pressure. Same physics, different lever.
Allison A. Bailes III, PhD is a speaker, writer, building science consultant, and the founder of Energy Vanguard in Decatur, Georgia. He has a doctorate in physics and is the author of a bestselling book on building science. He also writes the Energy Vanguard Blog. For more updates, you can follow Allison on LinkedIn and subscribe to Energy Vanguard’s weekly newsletter and YouTube channel.
Related Articles
Five Fun Facts About Dew Point Temperature
Make Dew Point Your Friend for Humidity
Psychrometrics – Impenetrable Chart or Path to Understanding?
Comments are welcome and moderated. Your comment will appear below after approval. To control spam, we close comments after one year.

I am missing the point of the article. Are you implying that when both outdoor air temperature and pressure rise, the dewpoint goes up and thus dew will form due to the change in atmospheric pressure? I don’t think so. An increase in atmospheric pressure of 1″Hg (which is very high) would only increase the dewpoint by about 1 F (assuming 70 F air 50%RH) if the humidity mass fraction remained constant.
Roy: Sorry about that. No, I’m talking about much larger changes than that. I thought about this when I was using my compressor, which takes air at atmospheric pressure (14.7 psi) and takes it up to 100 psi or so. So it’s not just increasing the pressure by a small fraction but several times its starting value.
Thanks for the comment. I can always count on you for good thermodynamic feedback. I’ll add something about the scale of pressures to help make the point.
Yea, I have experienced the air compressor issue too. Most of our industrial air systems use some type of air dehumidification to avoid that problem.
Allison, I was a bit lost as well looking for the conundrum you clearly point out in the first paragraph: morning dew on grass. More often than not, this phenomenon is due to radiative cooling when the grass is exposed to the cold clear night sky and looses enough heat energy via radiation to drop it’s temperature below the current dew point.
Paul: The conundrum is that condensation forms on grass happens when the temperature goes down but condensation in a compressor when temperature goes up.
I understand, but the first paragraph made it sound as if morning dew was a conundrum.
Hi Allison – A few weeks ago, for my first Claude Code project, I made a psychrometric calculator tool that allows the user to input various variables (including elevation) and outputs the moisture removed or dehumidification required.
Here is the link:
https://overture-psychrometric-calculator.netlify.app/
Since I am a dehumidifier person at heart, the tool was created with that bias.
It is free and if anyone has suggestions to improve it, I’d be happy to implement them.
Best, Todd
Thanks, Todd. I’ll check it out.
Thank you for the discussion on temperatures as related to dew points. For buildings, especially roofs Paul points out radiant cooling as a critical factor that generates dew most clear sky evenings. That can drop the temperatures of the surface quickly below dew point and below freezing. Important in roof applications and safety in walking on a low slope “wet” membrane.