Boiling Point at Altitude Calculator

Find the boiling point of water at any altitude in °C, °F, or K.

Science °C + °F + K 6 presets
Rate this calculator · 5.0 (1)

Boiling point at altitude

Antoine equation × US Standard Atmosphere

Instructions — Boiling Point at Altitude Calculator

  1. Enter the altitude in metres, feet, kilometres, or miles.
  2. Pick a famous-spot preset (Denver, Mexico City, Lhasa, Everest) if you want a quick check.
  3. Read the boiling point in °C, °F, and K, plus the atmospheric pressure in four units.
  4. The headline unit can be switched between Celsius, Fahrenheit, and Kelvin.

The model assumes pure water under the US Standard Atmosphere. Real weather can shift pressure by 1–3% (±0.3–0.9 °C in boiling point).

Formulas

Pressure at altitude (US Standard Atmosphere, troposphere):

$$P(h) = P_0 \left(1 - \frac{0.0065 \cdot h}{288.15}\right)^{5.2561}$$

Antoine equation (water, 1–100 °C, P in mmHg):

$$\log_{10} P = A - \frac{B}{C + T}$$

Solve for boiling point:

$$T_{bp} = \frac{B}{A - \log_{10} P} - C$$

Constants: A = 8.07131, B = 1730.63, C = 233.426. Sea-level reference: P₀ = 101,325 Pa = 760 mmHg = 1 atm.

Reference

  • Sea level (0 m): 100.00 °C / 212.00 °F
  • 500 m (1,640 ft): 98.4 °C / 209.1 °F
  • 1,000 m (3,280 ft): 96.7 °C / 206.1 °F
  • 1,609 m (Denver, 5,280 ft): 94.7 °C / 202.5 °F
  • 2,240 m (Mexico City): 92.7 °C / 198.9 °F
  • 3,500 m (Lhasa): 88.6 °C / 191.4 °F
  • 5,364 m (Everest base camp): 82.5 °C / 180.5 °F
  • 8,849 m (Everest summit): 70.5 °C / 158.9 °F
  • Pressure cooker (15 psi gauge): 121 °C / 250 °F
  • Rule of thumb: boiling point drops about 1 °C per 295 m gain (1 °F per 540 ft)

Article — Boiling Point at Altitude Calculator

Boiling point at altitude calculator

Water boils at 100 °C (212 °F) at sea level, but the boiling point drops about 1 °C per 295 m (1 °F per 540 ft) of altitude gain. Denver at 1,609 m boils water at 94.7 °C. La Paz at 3,640 m boils water at 88.4 °C. The summit of Everest at 8,849 m boils water at just 70.5 °C — barely warm enough for a hot cup of tea.

The physics is straightforward: water boils when its vapour pressure equals the surrounding atmospheric pressure, and atmospheric pressure falls as you climb. Combine the US Standard Atmosphere with the Antoine vapour-pressure equation and you have a robust altitude-to-boiling-point calculator that matches measured values within about 0.2 °C up to 5,000 m.

Water boiling point at altitude

Water boiling point at altitude is the temperature at which water transitions to vapour under reduced atmospheric pressure. At sea level, where pressure is 1 atm (101,325 Pa, 760 mmHg), pure water boils at exactly 100 °C. Climb 1 km and pressure falls to about 887 mbar, and boiling drops to roughly 96.7 °C. The relationship is non-linear because both pressure-versus-altitude and vapour-pressure-versus-temperature are exponential.

The implication for cooking is that food cooks more slowly even with the lid on, because the maximum temperature water can reach is set by the boiling point. At 3,000 m a pot of boiling water sits at 90 °C, meaning eggs, beans, and pasta need 20–60% more time depending on what is being cooked.

Why altitude changes the boiling point

Boiling is a phase change governed by vapour pressure equilibrium. As water heats, its molecules gain kinetic energy and more of them escape into the vapour phase. The pressure those escaped molecules exert is the vapour pressure. When the vapour pressure equals the external atmospheric pressure, bubbles can form throughout the liquid — that is boiling.

At higher altitudes, fewer air molecules sit above any point on Earth, so atmospheric pressure is lower. The vapour pressure needs to match that lower pressure, which it does at a lower temperature. The relationship is captured by the Clausius–Clapeyron equation in differential form, or by the more practical empirical Antoine equation in everyday calculations.

Did you know

You can boil water at room temperature without any heating. Place a beaker in a vacuum chamber and pump it down to about 23 mmHg (3% of sea-level pressure). Water starts boiling at 25 °C. Freeze-drying technology — used for instant coffee, MREs, and pharmaceuticals — depends on exactly this trick: water evaporates from frozen samples at low pressure without ever passing through the liquid phase.

The boiling point altitude formula

Two equations chain together. The US Standard Atmosphere gives pressure as a function of altitude in the troposphere. The Antoine equation gives the temperature at which water's vapour pressure equals any given external pressure.

Boiling point at altitude formulas
P(h) = P₀ × (1 − 0.0065h/288.15)^5.2561 US Standard Atmosphere
log₁₀ P = A − B/(C + T) Antoine equation
A = 8.07131, B = 1730.63, C = 233.426 water, 1–100 °C, P in mmHg
T_bp = B/(A − log₁₀ P) − C solve for boiling point

A quick mental-math shortcut: boiling point drops about 0.34 °C per 100 m gain in the first kilometre, and slightly more per metre as altitude increases. In US units, that is about 1 °F per 540 ft from sea level to mid-elevations. Higher up the rate steepens because pressure falls exponentially.

Boiling point by elevation

Water boiling temperatures at common landmarks and cities, computed from the formulas above.

  • Sea level (0 m): 100.0 °C / 212.0 °F. Reference standard.
  • Denver (1,609 m / 5,280 ft): 94.7 °C / 202.5 °F. Mile-High City.
  • Bogotá (2,640 m): 91.7 °C / 197.1 °F. Colombian capital.
  • Mexico City (2,240 m): 92.7 °C / 198.9 °F. North American megacity.
  • Lhasa (3,656 m): 88.3 °C / 190.9 °F. Tibetan plateau.
  • La Paz (3,640 m): 88.4 °C / 191.1 °F. Highest capital city.
  • Mount Whitney (4,418 m): 85.5 °C / 185.9 °F. Highest peak in lower 48 US states.
  • Everest base camp (5,364 m): 82.5 °C / 180.5 °F.
  • Everest summit (8,849 m): 70.5 °C / 158.9 °F. Tea barely steeps.
Sea level
100.0 °C
1.000 atm
Everest
70.5 °C
0.333 atm

High-altitude cooking and baking

Two things change at altitude. Boiling water is cooler, so wet-cooking methods are slower. Atmospheric pressure is lower, which affects baking because rising dough expands more aggressively before the structure sets.

Boiling adjustments: extend cook times by 25% above 1,500 m, by 50% above 2,500 m, and double them above 3,500 m for tough foods like beans, dried legumes, and large potatoes. Pasta still cooks in roughly the same time because it needs less heat penetration, but it absorbs more water along the way and can become mushy if not watched.

Baking adjustments above ~900 m: reduce baking powder/soda by 25%, reduce sugar by 1–2 tablespoons per cup, and add 1–4 tablespoons of liquid per cup. Bake at slightly higher temperature (about 8–14 °C / 15–25 °F warmer) to set the crumb before over-rising collapses it.

Pressure cookers and vacuum chambers

A pressure cooker raises absolute pressure above atmospheric to lift the boiling point. A standard 15-psi gauge cooker holds about 2 atm absolute, where water boils at 121 °C (250 °F). The 21 °C extra cooks beans and tough cuts of meat in a fraction of the open-pot time, and is the basis of pressure canning for low-acid foods — 121 °C is hot enough to destroy Clostridium botulinum spores.

Altitude affects pressure canning too

USDA pressure-canning guides specify higher processing pressures above 1,000 ft because the atmospheric component of the gauge reading is reduced at altitude. At 5,000 ft above sea level, use 13 psi gauge instead of 11 psi for the same actual canner temperature. Skipping the correction can leave low-acid foods under-processed and unsafe.

Common altitude cooking mistakes

Tip

Above 2,000 m, soft-boiled eggs need a different recipe entirely. Water at 92 °C cannot reach the 71 °C white-set temperature internally in the standard 4–5 minutes because heat transfer is slower. Use a covered pot, add 30–60 seconds, and ice-bath immediately.

The first mistake is assuming higher heat means faster cooking. A pot at full burner with vigorously boiling water at 90 °C still cannot exceed 90 °C — extra flame just evaporates water faster, not cook food faster. The fix is to extend time, not crank heat.

The second mistake is ignoring the air-pressure side of baking. At altitude, gases trapped in dough expand more before the dough sets, so over-leavened cakes rise spectacularly and then collapse. Cut leavening, add liquid, and use a slightly hotter oven to firm structure before the rise outpaces it.

The third mistake is confusing weather pressure with altitude pressure. A storm at sea level can drop pressure 25 mmHg below standard, shifting boiling by about 1 °C. That is not enough to ruin cooking but it does explain why a recipe behaves differently on stormy days. Altitude effects dwarf weather effects above 1,500 m.

FAQ

Boiling happens when a liquid's vapour pressure equals the surrounding atmospheric pressure. At higher altitudes the air is thinner and atmospheric pressure drops, so water reaches that equality at a lower temperature. At Denver (1,609 m / 5,280 ft) water boils near 94.7 °C; at Everest summit it boils near 70.5 °C.
About 96.7 °C (206.1 °F). Atmospheric pressure at 1,000 m drops from 760 mmHg at sea level to about 674 mmHg, which corresponds to a roughly 3.3 °C boiling-point reduction via the Antoine equation.
Cooking times for boiling water increase because the lower boiling temperature transfers heat to food more slowly. Rule of thumb: at 1,500–2,000 m add 25–50% to boil-time recipes. At 2,500–3,000 m double the time for tougher items like beans or potatoes. Baking is more complex — flour, leavening, and liquid quantities also need adjustment.
Combine the US Standard Atmosphere pressure formula P(h) = 101,325 × (1 − 0.0065h/288.15)^5.2561 with the Antoine equation log₁₀ P = A − B/(C + T) rearranged to T = B/(A − log₁₀ P) − C. For water in the 1–100 °C range, A = 8.07131, B = 1730.63, C = 233.426 when P is in mmHg.
Marginally. Humid air is slightly less dense than dry air at the same pressure, which has a tiny indirect effect. The dominant variable is atmospheric pressure, set by altitude and weather. A passing low-pressure system can drop pressure by 2–3% and shift boiling point by 0.5–1 °C at any altitude.
Pressure cookers reverse the altitude effect. A 15-psi gauge cooker raises absolute pressure to about 2 atm, lifting water's boiling point to roughly 121 °C / 250 °F. That hotter water cooks food roughly 3× faster than open-pot boiling and is the basis of canning sterilisation.
Within about 0.2 °C for altitudes from 0 to 5,000 m under standard conditions. Above 5,000 m the troposphere model starts to lose accuracy, and at Everest summit the result can be off by 0.5–1 °C versus measured local values because actual pressure varies with weather, latitude, and season.
Yes — at sufficiently low pressure. At about 23 mmHg (3% of sea-level pressure) water boils at 25 °C. Vacuum chambers exploit this for freeze-drying coffee and pharmaceuticals: low pressure lets water evaporate without applying heat that would damage the product.