Barometric Formula:
From: | To: |
The barometric formula describes how atmospheric pressure decreases with altitude in an isothermal atmosphere. It's derived from the ideal gas law and hydrostatic equilibrium.
The calculator uses the barometric formula:
Where:
Explanation: The formula shows how pressure decreases exponentially with altitude, with the rate of decrease depending on temperature and the molar mass of air.
Details: Understanding pressure changes with elevation is crucial for aviation, meteorology, engineering, and scientific research. It affects weather patterns, aircraft performance, and even human physiology at high altitudes.
Tips:
Q1: Why does pressure decrease with altitude?
A: Pressure decreases because there's less atmospheric mass above pushing down at higher elevations.
Q2: How accurate is this formula?
A: It's accurate for an isothermal atmosphere. Real atmospheres have temperature variations, so this is an approximation.
Q3: What's the pressure at Mount Everest's summit?
A: About 32,000 Pa (vs 101,325 Pa at sea level) for standard conditions (8848m, T=229K).
Q4: Does humidity affect the calculation?
A: Yes, humid air has slightly lower molar mass (water is lighter than N₂/O₂), but this calculator uses dry air values.
Q5: Can this be used for other planets?
A: Yes, with appropriate values for P₀, M, g, and T for that planet's atmosphere.