Altitude from Pressure Equation:
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The altitude from pressure equation calculates height above sea level based on atmospheric pressure measurements. It's derived from the barometric formula and is widely used in aviation, meteorology, and aerospace applications.
The calculator uses the following equation:
Where:
Explanation: The equation models the atmosphere's pressure decrease with altitude under the assumption of a constant temperature lapse rate.
Details: Accurate altitude determination is crucial for aircraft navigation, weather forecasting, and scientific research. It's also used in various engineering applications where atmospheric conditions affect performance.
Tips: Enter all parameters in the correct units. Default values are provided for standard atmospheric conditions (T0=288.15K, P0=101325Pa, L=0.0065K/m, R=287.05J/kg·K, g=9.80665m/s²).
Q1: What are typical values for the temperature lapse rate?
A: In the troposphere (up to 11km), the standard lapse rate is about 0.0065 K/m, but it can vary with weather conditions.
Q2: How accurate is this calculation?
A: It provides good estimates under standard atmospheric conditions but may have errors in extreme weather or non-standard atmospheres.
Q3: Can I use this for very high altitudes?
A: This equation works best for altitudes within the troposphere (up to about 11km). Different models are needed for higher altitudes.
Q4: Why does temperature affect altitude calculation?
A: Warmer air is less dense, causing pressure to decrease more slowly with altitude. The lapse rate accounts for this temperature variation.
Q5: What's the difference between geometric and geopotential altitude?
A: This calculator gives geometric altitude. Geopotential altitude accounts for gravity variation with height and is used in some atmospheric models.