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05 Water, Air and Heat

Elevation to Pressure Calculator: What It Shows

Card No. 05·0537 · Updated · Standard formula, shown below

Estimated pressure 89.87 kPa
Estimated pressure
898.7 hPa
Result
Estimated pressure
26.54 inHg
Result
Elevation
1000 m
You entered
You enter
Elevation
You get
Estimated pressure, Estimated pressure, Estimated pressure
Rounding
2 dp · 1 dp

An elevation-to-pressure calculator estimates atmospheric pressure at a specified height above sea level, using a standard-atmosphere model. Enter elevation in metres or feet, and it returns estimated pressure in kilopascals, hectopascals, or inches of mercury; actual local pressure can differ with weather and temperature.

Formula

This calculator uses the barometric formula for the standard atmosphere in the troposphere:

p = 101.325 × (1 − h / 44,330)5.25588

  • p is estimated absolute atmospheric pressure in kilopascals (kPa).
  • h is elevation above mean sea level in metres (m).
  • 101.325 kPa is the standard-atmosphere pressure at sea level.
  • 44,330 m and the exponent 5.25588 are constants in this approximate standard-atmosphere relationship.

The other outputs convert the same pressure: 1 kPa equals 10 hPa, and 1 kPa is approximately 0.2953 inches of mercury (inHg). The input range ends at 44,330 m because the expression reaches zero there; the simple formula is not a suitable atmospheric model at or above that height.

Worked Example

Using the calculator’s default elevation of 1,000 m:

  1. Find the height fraction: 1,000 ÷ 44,330 ≈ 0.02256.
  2. Subtract it from 1: 1 − 0.02256 ≈ 0.97744.
  3. Raise the result to 5.25588 and multiply by 101.325: 101.325 × 0.977445.25588 ≈ 90.08 kPa.
  4. Convert units: 90.08 × 10 ≈ 900.8 hPa; 90.08 × 0.2953 ≈ 26.60 inHg.

So the estimated pressure at 1,000 m is 90.08 kPa, or about 900.8 hPa and 26.60 inHg. These are equivalent ways of expressing the model’s estimate, not separate measurements.

How Elevation Changes Pressure

Air has weight. The atmosphere above a location presses on the air below it, so a person at higher elevation generally has less air overhead and experiences lower atmospheric pressure. The decrease is not a fixed amount per metre: pressure falls more rapidly near sea level than it does higher in the atmosphere because air density also decreases with height.

At sea level, the standard atmosphere is 101.325 kPa, equal to 1,013.25 hPa or approximately 29.92 inHg. At 1,000 m, the calculator’s standard estimate is about 90.08 kPa. These reference values describe a model, not a promise that a weather station will show exactly the same number.

Elevation should mean height above mean sea level, not height above a nearby road, valley floor, or building entrance. If a location is 600 m above sea level, enter 600 even if it is only 80 m above the local valley.

When to Use the Estimate

This calculation is useful for understanding how pressure changes with altitude, making a rough comparison between locations, or getting a reference value when no live weather observation is available. It can also help explain why pressure readings and weather reports use different units.

It estimates static atmospheric pressure—the surrounding air pressure at a location. It does not calculate pressure inside a container, a fluid’s pressure at depth, or the pressure difference created by moving air. Those questions require additional information and different equations.

For a current local atmospheric pressure, use a nearby weather station or a properly configured barometer. Check whether its value is station pressure or sea-level-adjusted pressure. Weather services often adjust observations to sea level so places at different heights can be compared; that adjusted figure is not the same as the pressure actually present at the elevated location.

Units, Inputs, and Common Mistakes

  • Convert feet to metres: divide feet by 3.28084, or multiply by 0.3048. For example, 3,281 ft is about 1,000 m.
  • Keep pressure units distinct: 1 kPa = 10 hPa = 10 mbar. InHg is another common unit; do not read a value in hPa as if it were inHg.
  • Do not confuse altitude with pressure altitude: aviation pressure altitude is based on an altimeter setting and a reference atmosphere; it is not simply a location’s surveyed elevation.
  • Avoid overinterpreting decimals: two decimal places in kPa are display precision, not a claim that real local pressure is known that precisely.

Make sure the elevation is entered in metres: entering a feet value directly can produce a substantially incorrect result. Also distinguish absolute pressure from gauge pressure. Atmospheric pressure is an absolute pressure referenced to a vacuum; gauge pressure is measured relative to surrounding air and can be zero while the atmosphere is still exerting pressure.

Model Limits and Real-World Pressure

The standard-atmosphere equation assumes a simplified vertical temperature profile and representative atmospheric conditions. Real air pressure changes with weather systems, temperature, humidity, and local conditions. A high- or low-pressure weather system can shift a measured reading away from the calculator’s estimate even when the elevation is entered correctly.

The formula is intended for the lower atmosphere and is commonly used as a standard approximation through the troposphere. It should not be extrapolated to high-altitude or spaceflight conditions, where atmospheric layers and temperature profiles require more detailed models. It also does not predict short-term weather or provide a calibrated instrument reading.

For work where an exact pressure matters, use a current measurement and the relevant technical standard or model. A calculator estimate is useful context, but it cannot replace site-specific data or professional guidance when pressure affects equipment or an operational decision.

Frequently Asked Questions

What is the air pressure at sea level?
The standard-atmosphere reference is 101.325 kPa, or 1,013.25 hPa, approximately 29.92 inHg. Actual sea-level pressure changes with weather.

How much does pressure drop per 1,000 feet?
There is no single fixed drop per 1,000 ft because pressure changes nonlinearly with elevation. Near sea level, the standard model gives a larger decrease per unit of height than it does at higher elevations.

Does elevation mean height above sea level?
Yes. This calculator expects elevation above mean sea level. Height above a nearby surface is not enough unless you also know that surface’s elevation.

Why does my barometer show a different pressure?
The calculator gives a standard-atmosphere estimate, while a barometer measures local conditions. Weather, instrument calibration, and whether a report is adjusted to sea level can all explain a difference.

Can I enter feet instead of metres?
Convert feet to metres first: multiply the feet value by 0.3048. For example, 5,000 ft is 1,524 m.

Is this pressure absolute or gauge pressure?
It is absolute atmospheric pressure. Gauge pressure is pressure relative to the surrounding atmosphere and requires a separate reference measurement.

Related

Formula used
in h | Elevation | m | 1000 | 0 | 44330
out p | Estimated pressure | kPa | 101.325 * (1 - h / 44330)^5.25588 | 2
out hp | Estimated pressure | hPa | p * 10 | 1
out inhg | Estimated pressure | inHg | p * 0.2953 | 2

Each line is one input (in, sel, list) or one result (out: label, unit, formula, decimals). How the calculators work

Method: the standard formula for this calculation, rounded as each result states. See how the calculators work or report an error.

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