Atmospheric Pressure Formula:
From: | To: |
Atmospheric pressure is the force per unit area exerted by the weight of the atmosphere above a surface. It is commonly measured using a barometer, which typically contains a fluid column whose height varies with pressure changes.
The barometer works based on the hydrostatic pressure formula:
Where:
Explanation: The atmospheric pressure balances the weight of the fluid column, allowing us to calculate pressure from the height measurement.
Details: Accurate atmospheric pressure measurement is crucial for weather forecasting, aviation, industrial processes, and scientific research. It helps predict weather patterns and ensure safety in various applications.
Tips: Enter the fluid density in kg/m³ (mercury density is approximately 13595 kg/m³), gravity in m/s² (standard is 9.81 m/s²), and the height of the fluid column in meters. All values must be positive.
Q1: Why is mercury commonly used in barometers?
A: Mercury has a high density, which means the column height is manageable (about 0.76m at sea level) and provides precise measurements.
Q2: What are the units of atmospheric pressure?
A: Common units include Pascals (Pa), atmospheres (atm), millimeters of mercury (mmHg), and bars (bar). This calculator uses Pascals.
Q3: How does altitude affect atmospheric pressure?
A: Atmospheric pressure decreases with increasing altitude as there is less air above to exert pressure.
Q4: Can water be used in barometers?
A: Yes, but water's lower density requires a much taller column (about 10.3m at sea level), making it less practical than mercury.
Q5: How does temperature affect barometer readings?
A: Temperature affects fluid density and expansion. Most barometers include temperature compensation for accurate readings.