Estimate temperature changes based on altitude using lapse rate formulas.
Custom Rate
Average Environment
Dry Adiabatic (Unsaturated)
Moist Adiabatic (Saturated)
Rate of cooling per 1000 m
Please enter valid numerical values.
Estimated Temperature at Target Altitude
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How to Calculate Temperature Using Lapse Rate
The lapse rate is defined as the rate at which atmospheric temperature decreases with an increase in altitude. Understanding this concept is crucial for meteorology, aviation, mountain climbing, and predicting weather patterns. This calculator helps you determine the expected temperature at a specific elevation based on a starting temperature and the atmospheric conditions.
The Calculation Formula
The general physics formula used to calculate the temperature at a new altitude is:
Tfinal = Tstart – (L × Δh)
Tfinal: The temperature at the target altitude.
Tstart: The known temperature at the starting altitude (often sea level).
L: The Lapse Rate (rate of cooling). Note that while temperature generally drops, mathematically the rate is usually expressed as a positive number representing the drop per unit distance.
Δh: The difference in altitude (Target Altitude – Starting Altitude).
Standard Lapse Rate Values
Depending on humidity and atmospheric stability, the rate at which air cools changes. Here are the standard values used in this calculator:
Condition
Metric Rate (Approx.)
Imperial Rate (Approx.)
Environmental Lapse Rate (Average)
6.5°C per 1,000 meters
3.56°F per 1,000 feet
Dry Adiabatic Lapse Rate (DALR)
9.8°C per 1,000 meters
5.38°F per 1,000 feet
Moist Adiabatic Lapse Rate (MALR)
~5.0°C per 1,000 meters
~2.7°F per 1,000 feet
Definitions of Inputs
Starting Temperature: The thermometer reading at your current location or base level.
Starting & Target Altitude: The elevation above sea level for your start and end points. If you are starting at sea level, enter 0.
Dry Adiabatic: Used when air is unsaturated (relative humidity is less than 100%). Air cools faster in dry conditions.
Moist Adiabatic: Used when air is saturated (in clouds/fog). The release of latent heat during condensation causes the air to cool more slowly.
Real World Example
Imagine you are hiking. The temperature at the trailhead (500 meters) is 25°C. You are hiking to a peak at 2,500 meters. Assuming a standard environmental lapse rate of 6.5°C/km: