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Atmospheric Pressure Calculator

Atmospheric Pressure Equation:

\[ P = P_0 \times e^{\left(\frac{-Mgh}{RT}\right)} \]

Pa
kg/mol
meters
Kelvin

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1. What is the Atmospheric Pressure Equation?

The atmospheric pressure equation calculates the pressure at a given altitude based on the barometric formula. It describes how atmospheric pressure decreases exponentially with altitude.

2. How Does the Calculator Work?

The calculator uses the barometric formula:

\[ P = P_0 \times e^{\left(\frac{-Mgh}{RT}\right)} \]

Where:

Explanation: The equation accounts for the exponential decrease in pressure with altitude due to the weight of the air column above.

3. Importance of Pressure Calculation

Details: Atmospheric pressure calculations are essential for aviation, meteorology, engineering, and understanding weather patterns and human physiology at different altitudes.

4. Using the Calculator

Tips: Enter sea level pressure (default is standard 101325 Pa), molar mass of air (default 0.02896 kg/mol), altitude in meters, and temperature in Kelvin. All values must be positive.

5. Frequently Asked Questions (FAQ)

Q1: Why does pressure decrease with altitude?
A: Pressure decreases because there's less atmospheric mass above you as you go higher, resulting in less weight pushing down.

Q2: What is standard sea level pressure?
A: The standard atmospheric pressure at sea level is 101325 Pa (1013.25 hPa or 1 atm).

Q3: How does temperature affect atmospheric pressure?
A: Warmer air expands and becomes less dense, leading to lower pressure at a given altitude compared to colder conditions.

Q4: What is the molar mass of dry air?
A: The molar mass of dry air is approximately 0.02896 kg/mol (28.96 g/mol).

Q5: How accurate is this calculation?
A: This provides a theoretical estimate. Real atmospheric pressure varies with weather conditions, humidity, and local geography.

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