Temperature at Altitude Calculator

Calculate temperature at altitude and temperature change based on reference temperature, reference altitude, target altitude, and lapse rate. Temperature at Altitude Calculator helps pilots, engineers, students, and meteorologists estimate atmospheric conditions across elevations.

Highlights

  • Estimate atmospheric temperature at any altitude.
  • Calculate temperature changes between two elevations.
  • Supports Celsius, Fahrenheit, and Kelvin.
  • Works with meters, kilometers, feet, miles, and nautical miles.
  • Use standard or custom atmospheric lapse rates.

Table of Contents

  1. How Temperature at Altitude Calculator Works?
  2. Practical Use Cases
  3. Accuracy and Limitations
  4. Quick Examples
  5. Frequently Asked Questions (FAQs)
  6. Cite This Calculator

How Temperature at Altitude Calculator Works?

The Temperature at Altitude Calculator uses a linear atmospheric lapse-rate model. It starts with a known reference temperature and adjusts it according to the difference between the reference altitude and the target altitude.

Ttarget=Tref−L⁢(htarget−href)

In this equation, Ttarget is the estimated temperature at the target altitude, Tref is the reference temperature, L is the temperature lapse rate, and htarget and href are the target and reference elevations. A positive lapse rate means temperature decreases as altitude increases. A negative lapse rate represents temperature increasing with altitude.

The calculator also reports the temperature change separately:

ΔT=Ttarget−Tref=−L⁢(htarget−href)

For example, with a reference temperature of 15 °C at 0 m, a target altitude of 1.5 km, and a lapse rate of 6.5 °C/km, the estimated temperature change is −9.75 °C and the temperature at the target altitude is 5.25 °C.


Input or outputMeaningSupported choices
Reference TemperatureKnown temperature at the reference elevation°C, °F, K
Reference and Target AltitudeElevations used to determine the altitude differencem, km, ft, mi, nmi
Temperature Lapse RateTemperature change per elevation increase°C/km, °C/m, K/km, K/m, °F/1000 ft, °F/ft
ResultsEstimated target temperature and temperature difference°C, °F, K

Practical Use Cases

Pilots: Pilots can estimate the outside-air temperature at a planned cruising or approach altitude from a known airport or weather-observation temperature. This helps with basic performance planning and anticipating atmospheric conditions.

Engineers: Engineers can model approximate temperature conditions at elevated construction sites, towers, pipelines, or other infrastructure locations when evaluating environmental loads and operating conditions.

Students: Students can use the calculator to verify atmospheric physics exercises involving reference temperature, elevation differences, and standard or custom lapse rates.

Meteorologists: Meteorologists can make a quick first-order estimate of temperature at another elevation using a measured station temperature and an assumed lapse rate before applying more detailed atmospheric data.

Accuracy and Limitations

The calculator provides a linear estimate based only on the supplied reference temperature, two elevations, and lapse rate. It does not model temperature inversions, changing lapse rates, humidity, pressure, cloud layers, solar heating, terrain effects, or local weather systems, so results may differ substantially from observations, especially across large elevation ranges or outside the lower atmosphere. The result is most representative when the selected lapse rate is appropriate for the specific atmospheric layer and the input values are measured accurately; the supported input ranges are −100 to 100 °C, −1000 to 100000 for altitude, and −20 to 20 for the lapse-rate value in its selected form.

Quick Examples

Example #1: Standard Sea-Level Estimate

Estimate the temperature at a moderate elevation using standard atmospheric conditions.

Example #2: High-Altitude Aviation

Calculate atmospheric cooling from a low-altitude reference point to a high cruising altitude.

Example #3: Mountain Weather Comparison

Estimate the temperature change between a mountain station and a higher summit.

Frequently Asked Questions

In the lower atmosphere, temperature usually decreases as altitude increases. A commonly used average rate is about 6.5°C per kilometer.

A temperature lapse rate describes how much air temperature changes over a given increase in altitude. It can vary depending on atmospheric conditions, location, and weather patterns.

Air pressure decreases with altitude, allowing rising air to expand and cool. This is why mountainous areas are often colder than nearby lowland regions.

Pilots can use estimated temperatures to support flight planning, assess aircraft performance, and anticipate atmospheric conditions at different elevations.

No. The standard lapse rate is an average reference value, while actual temperature changes may differ because of humidity, inversions, weather systems, and local terrain.

Cite This Calculator