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Boiling Point Calculator

Water's boiling point at altitude, from the pressure.

Water's boiling point at altitude, from the pressure.

Written and maintained by Mohit PatelLast checked August 4, 2026How we build these
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Boiling point (°C)

100

212 °F · 101.325 kPa

Boiling point100 °C
In Fahrenheit212 °F
Air pressure101.325 kPa
Below sea-level boiling0 °C
Rough cooking time factor1×

Water boils when its vapour pressure matches the air above it, so lower pressure means a lower boiling point. This uses the Clausius-Clapeyron relation against the standard atmosphere rather than the "1 °C per 285 m" rule of thumb, which is a linearisation that drifts at altitude. The cooking factor is a rough guide from the rule that reaction rates roughly double every 10 °C — it is why Denver needs longer for eggs and why pressure cookers exist.

How the Boiling Point Calculator works

Water boils when its vapour pressure matches the air above it, so lower pressure means a lower boiling point. This uses the Clausius-Clapeyron relation against the standard atmosphere rather than the familiar 1 °C per 285 m rule, which is a linearisation that drifts at altitude.

Also known as: boiling point at altitude · water boiling point by elevation · high altitude cooking calculator · boiling point by pressure

Where to go next

The Boiling Point question rarely arrives on its own. These are the ones that usually come with it:

Frequently asked questions

At what temperature does water boil at altitude?

About 95 °C in Denver at 1,609 m, and near 71 °C on Everest. The drop accelerates with height as the air thins.

Why does food take longer to cook at altitude?

Because the water is cooler, not because it boils more slowly. Reaction rates roughly double every 10 °C, so cooking at 95 °C rather than 100 °C takes noticeably longer.

How does a pressure cooker help?

By raising the pressure above the surrounding air, which raises the boiling point above 100 °C. That is the same mechanism working in reverse.

Does the rule of 1 °C per 285 m work?

Roughly, near sea level. It is a straight-line approximation to a curve, so it drifts at height, which is why this page computes from the pressure instead.

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