Atmospheric Pressure Equation:
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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.
The calculator uses the equation:
Where:
Explanation: The equation models how atmospheric pressure decreases with altitude, accounting for the temperature change rate.
Details: Accurate pressure calculation is crucial for aviation, meteorology, engineering, and scientific research at different altitudes.
Tips: Enter all required values with correct units. Default values are set for standard Earth atmosphere at sea level.
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.