Atmospheric Pressure Formula:
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The atmospheric pressure formula calculates how pressure decreases with altitude in an isothermal atmosphere. It's derived from the barometric formula and assumes constant temperature throughout the atmospheric layer.
The calculator uses the atmospheric pressure formula:
Where:
Explanation: The formula shows how atmospheric pressure decreases exponentially with height, with the rate of decrease depending on air properties and temperature.
Details: Calculating atmospheric pressure at different altitudes is crucial for aviation, meteorology, engineering design, and understanding weather patterns and climate science.
Tips: Enter reference pressure in Pascals, height in meters, molar mass in kg/mol, gravity in m/s², gas constant in J/mol·K, and temperature in Kelvin. Default values represent standard Earth conditions.
Q1: Why does pressure decrease with altitude?
A: Pressure decreases with altitude because there's less air above pushing down, and gravity's effect on air molecules diminishes with height.
Q2: What are typical sea level pressure values?
A: Standard atmospheric pressure at sea level is 101,325 Pa (1013.25 hPa or 29.92 inches of mercury).
Q3: How does temperature affect atmospheric pressure?
A: Warmer temperatures generally result in lower pressure at a given altitude as air expands and becomes less dense.
Q4: What are the limitations of this formula?
A: This formula assumes constant temperature, which isn't accurate for large altitude changes where temperature varies significantly.
Q5: Can this formula be used on other planets?
A: Yes, with appropriate values for gravitational acceleration, molar mass of the atmosphere, and temperature.