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Boiling Point and Altitude

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Pick a mode (altitude to boiling point, boiling point to altitude, or pressure to boiling point) and the right-hand side gives altitude, pressure and boiling point, with a cooking-time correction when you want one. ⚠️ Pressure uses the International Standard Atmosphere (ISA), not linear interpolation. `P = 101.325 × (1 − 2.25577e-5 × h)^5.25588` in kPa, within the troposphere. Pressure falls exponentially with altitude, so linear interpolation is several degrees out at 3,000 m — the true value is about 89.9 °C, while a straight line lands around 90. ⚠️ The boiling point uses a Clausius–Clapeyron approximation. `ln(P/P₀) = −(ΔHvap / R)(1/T − 1/T₀)`, anchored at sea level (101.325 kPa → 100.00 °C). The latent heat is taken as 41.1 kJ/mol, the value for water near 90–100 °C. ⚠️ At altitude 0 the result must be 100 °C. That anchor is what shows whether the formula has drifted, and a test pins it. Cooking times are an empirical range, not a precise value, and sterilising at altitude cannot be fixed by time alone (it needs a pressure canner).

Features

  • Three modes: altitude to boiling point, boiling point to altitude, pressure to boiling point
  • ⚠️ Pressure from the International Standard Atmosphere (ISA), not linear interpolation
  • ⚠️ Boiling point from a Clausius–Clapeyron approximation with consistent, sourced constants
  • ⚠️ Anchors pinned: altitude 0 → 100.00 °C, and 3,000 m ≈ 89.9 °C
  • Gives the pressure, temperature and boiling point at that place
  • Cooking-time correction (noodles / rice / sterilisation) as an empirical range
  • ⚠️ Notes that sterilising at altitude needs a pressure canner, not just more time
  • Computed locally with no network requests

How to use

  1. Pick a mode (from altitude, from boiling point, or from pressure)
  2. Enter the matching value (metres, degrees Celsius, or kPa)
  3. Optionally pick a cooking-time correction (none / noodles / rice / sterilisation)
  4. The right-hand side gives altitude, pressure, boiling point and how much longer to cook

FAQ

At what temperature does water boil at 3,000 m?
About 89.9 °C. Under the Standard Atmosphere the pressure at 3,000 m is roughly 70.1 kPa, and the Clausius–Clapeyron approximation gives 89.9 °C. Note that you cannot linearly interpolate between the 100 °C at sea level and some higher point: pressure falls exponentially with altitude, so a straight line is more than 1 °C out at 3,000 m. This is the tool’s default example — open it and check.
Why does cooking take longer at altitude?
Because the boiling point drops. Most cooking reactions speed up with temperature, and when water boils at 90 °C rather than 100 °C the food cannot reach 100 °C internally, so reactions and starch gelatinisation slow down. Empirically the time rises by tens of percent, more so the higher you are. The tool gives a range based on “a few percent longer per degree the boiling point falls” — it varies with the food, the pan and the stove, so it was never a precise value.
How do you sterilise water at altitude?
Time alone is not enough. Boiling does kill bacteria and viruses, but at 90 °C water cannot reliably kill certain spores (such as botulinum), so canning and similar tasks needing a higher temperature call for a pressure canner, which raises the boiling point back above 100 °C. The “sterilisation” correction here only gives the empirical time range and flags this point — time cannot solve a temperature ceiling.

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