Barometric Formula:
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The barometric formula describes how atmospheric pressure changes with temperature in an ideal gas atmosphere. It provides a mathematical relationship between pressure and temperature under specific atmospheric conditions.
The calculator uses the barometric formula:
Where:
Explanation: The formula accounts for how atmospheric pressure varies with temperature changes in an ideal gas atmosphere, considering gravitational effects and gas properties.
Details: Accurate pressure calculation is crucial for meteorological forecasting, aviation, engineering applications, and understanding atmospheric phenomena. It helps in predicting weather patterns and designing pressure-sensitive systems.
Tips: Enter reference pressure in Pascals, temperatures in Kelvin, and molar mass in kg/mol. The default molar mass value (0.02896 kg/mol) represents dry air. All values must be positive and non-zero.
Q1: What is the typical reference pressure at sea level?
A: Standard atmospheric pressure at sea level is approximately 101,325 Pa (1013.25 hPa).
Q2: Why use Kelvin instead of Celsius?
A: Kelvin is an absolute temperature scale required for thermodynamic calculations, as it starts from absolute zero and ensures positive values in exponential functions.
Q3: What is the molar mass of dry air?
A: The molar mass of dry air is approximately 0.02896 kg/mol, which accounts for the mixture of nitrogen, oxygen, and other gases.
Q4: Are there limitations to this formula?
A: This formula assumes an ideal gas atmosphere and constant temperature lapse rate. It may be less accurate in extreme atmospheric conditions or when humidity effects are significant.
Q5: How does temperature affect atmospheric pressure?
A: Generally, as temperature increases, air expands and becomes less dense, which can lead to lower pressure at a given altitude under certain conditions.