Barometric Pressure Equation:
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The barometric pressure equation calculates atmospheric pressure at a given height above sea level. It's derived from the ideal gas law and hydrostatic equation, describing how pressure decreases exponentially with altitude.
The calculator uses the barometric pressure equation:
Where:
Explanation: The equation assumes constant temperature and gravitational acceleration, providing an exponential decrease in pressure with altitude.
Details: Accurate pressure calculation is crucial for meteorology, aviation, altitude measurements, and understanding atmospheric phenomena. It helps in weather forecasting, aircraft performance calculations, and scientific research.
Tips: Enter initial pressure in Pascals, gravitational acceleration in m/s² (default is Earth's gravity 9.80665), height in meters, gas constant in J/(kg·K) (default for dry air is 287.058), and temperature in Kelvin. All values must be positive.
Q1: Why does pressure decrease with altitude?
A: Pressure decreases because there's less atmospheric mass above higher elevations, resulting in lower weight of air column.
Q2: What are typical values for P₀ at sea level?
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 pressure calculation?
A: Higher temperatures result in less rapid pressure decrease with altitude, as warmer air is less dense.
Q4: What are the limitations of this equation?
A: The equation assumes constant temperature and gravity, and doesn't account for humidity, which can affect actual pressure profiles.
Q5: Can this be used for other planets?
A: Yes, with appropriate values for gravitational acceleration and gas constant for the specific planetary atmosphere.