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Calculate Atmospheric Pressure From Elevation and Temperature

Atmospheric Pressure Equation:

\[ P = P_0 \times \left(\frac{T_0}{T_0 + L h}\right)^{\frac{g M}{R L}} \]

Pa
K
K/m
m
m/s²
kg/mol
J/(mol·K)

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1. What is the Atmospheric Pressure Equation?

The atmospheric pressure equation calculates pressure at a given elevation considering temperature lapse rate. It's derived from the barometric formula and accounts for changes in temperature with altitude.

2. How Does the Calculator Work?

The calculator uses the equation:

\[ P = P_0 \times \left(\frac{T_0}{T_0 + L h}\right)^{\frac{g M}{R L}} \]

Where:

Explanation: The equation models how atmospheric pressure decreases with altitude, accounting for the temperature change rate.

3. Importance of Pressure Calculation

Details: Accurate pressure calculation is crucial for aviation, meteorology, engineering, and scientific research at different altitudes.

4. Using the Calculator

Tips: Enter all required values with correct units. Default values are set for standard Earth atmosphere at sea level.

5. Frequently Asked Questions (FAQ)

Q1: What are typical values for the lapse rate (L)?
A: On Earth, the average tropospheric lapse rate is about 0.0065 K/m, but it varies with atmospheric conditions.

Q2: Why does temperature affect pressure with altitude?
A: Warmer air expands, making the pressure decrease more slowly with altitude. Colder air contracts, making pressure decrease faster.

Q3: What's the standard sea level pressure?
A: The international standard atmosphere defines sea level pressure as 101325 Pa (1 atm).

Q4: When is this equation not valid?
A: In very high altitudes where the atmosphere becomes non-ideal, or when temperature doesn't change linearly with altitude.

Q5: How does this differ from the simple barometric formula?
A: This version accounts for temperature changes with altitude, while the simple barometric formula assumes constant temperature.

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