How the result is calculated
Altitude and boiling-point equations
P = 101325 × (1 − 2.25577×10⁻⁵h)^5.25588; T = 1663.125 ÷ (5.08354 − log₁₀(Pbar)) + 45.622 − 273.15
The first equation estimates standard atmospheric pressure from altitude h in meters in the troposphere. The second inverts NIST’s Antoine vapor-pressure equation for water using its 344–373 K coefficient set. The result is an estimate: weather pressure, thermometer accuracy, latitude, and local conditions can shift an observed boil.
Worked example: brewing at 5,000 ft
- Convert 5,000 ft to meters: 5,000 × 0.3048 = 1,524 m.
- The standard-atmosphere equation estimates local pressure near 84 kPa.
- The water vapor-pressure equation gives an estimated boiling point near 95°C / 203°F.
- That is above Sencha’s 70–80°C starting range, so boil and cool; it may be below the hottest end requested by some black-tea recipes.


