Altitude From Pressure

Invert the barometric formula to estimate altitude from measured atmospheric pressure.

Description

Invert the barometric formula to estimate altitude from measured atmospheric pressure.

Altitude From Pressure is a focused chemistry tool that invert the barometric formula to estimate altitude from measured atmospheric pressure. It calculates locally from the values you enter and exposes the result without changing the source observations.1

When to use Altitude From Pressure

Use Altitude From Pressure when you need to invert the barometric formula to estimate altitude from measured atmospheric pressure. Enter Pressure and Temperature using the definitions and units below so the result can be reproduced.

Pressure
A finite measured or assumed value, expressed in hPa.
Temperature
A finite measured or assumed value, expressed in K.

How Altitude From Pressure calculates the result

The published tool contract uses this rule: Invert the barometric formula to estimate altitude from measured atmospheric pressure.

Altitude
The calculated altitude in m.

Limitations of Altitude From Pressure

The output is an estimate tied to the stated model and coefficients; it is not a direct measurement and should retain that label when reported.

Alternative or Complementary measurements

Retain the original Pressure and Temperature values and their units alongside the result. Barometric Pressure is useful when you instead need to estimate atmospheric pressure at altitude from temperature using the barometric formula. Dewpoint From Vapor Pressure provides another view by helping you invert the Magnus formula to compute dewpoint temperature from water vapor pressure.

References

  1. Pressure altitude — Wikipedia contributors

Similar or alternative tools

  • Barometric Pressure

    Estimate atmospheric pressure at altitude from temperature using the barometric formula.

  • Dewpoint From Vapor Pressure

    Invert the Magnus formula to compute dewpoint temperature from water vapor pressure.

  • Clausius–Clapeyron Vapor Pressure

    Estimate vapor pressure at a second absolute temperature from a reference pressure and molar enthalpy of vaporization using the integrated Clausius–Clapeyron equation. Assumes vapor behaves ideally and enthalpy stays constant over the temperature interval.

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