The short answer, with the caveat attached
Under 55°F and almost nobody notices the air. Between 55 and 60°F it is still comfortable. From 60°F it starts to feel present, by 65°F it is muggy to most people, and past 70°F it is oppressive.
The caveat matters more than usual here, because comfort is the one thing on this site that is not purely physics. Someone who has spent a summer in Houston will find 68°F ordinary; someone who has spent it in Denver will find it brutal. The bands are the middle of a wide distribution.
Why the threshold is a dew point and not a percentage
You can sweat in 90% humidity and be perfectly comfortable, or be miserable at 50%. Neither is a paradox once you know the temperature.
Comfort in warm weather is about whether sweat can evaporate, and evaporation is driven by the difference between the water at your skin and the water already in the air. What matters is therefore the amount of water in the air — which the dew point measures directly, and which the percentage only measures relative to a moving ceiling.
| Air temperature | Dew point | How it feels |
|---|---|---|
| 55°F | 41°F | Dry and cool. Nothing to notice. |
| 75°F | 60°F | Warm, slightly close. Pleasant enough. |
| 95°F | 79°F | Punishing. Sweat runs without cooling. |
Same percentage, three completely different days — which is the whole reason dew point beats humidity as a comfort measure.
What each threshold actually changes
The bands are not arbitrary points on a scale of unpleasantness. Each corresponds to something observable:
- 55°F — laundry outdoors dries in an afternoon. Finishes cure overnight without trouble.
- 60°F — the first point at which people spontaneously mention the humidity. Overnight lows stop falling much below this.
- 65°F — mild exertion produces sweat that does not evaporate. Glasses fog on stepping outside from air conditioning.
- 70°F — nights stay warm and uncomfortable, because air cannot cool below its own dew point. Sleep quality drops measurably for most people.
- 75°F — genuinely tropical. Rare outside the deep subtropics.
The cold end
The scale above is about summer, and it stops being useful in winter, when the question reverses: the air is not too full but too empty.
Below a dew point of about 30°F the air is dry enough to draw water out of everything it touches. That is where static shocks, cracked lips and dry sinuses come from, and it is why heated indoor air in a cold climate is so dry: cold outdoor air holds very little water, and warming it does not add any.
Where to see today's
The dew point chart has the full scale in both units with a printable grid, and the calculator converts a temperature and humidity if that is what you have. For the current outdoor figure where you are, use humidity today.