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Atmospheric Pressure:

  • Definition: Atmospheric pressure is the force exerted by the weight of air (and water vapor) on a unit area at a given point. It is the pressure exerted by the Earth’s atmosphere on everything within it.
  • Measurement:
  • At Sea Level:
    • In psi (Pounds per Square Inch): Approximately 14.7 psi absolute.
    • In mmHg (Millimeters of Mercury): 760 mmHg.
    • In kPa (Kilopascals): 101.3 kPa.
  • Variation with Altitude: Atmospheric pressure decreases with altitude. At higher elevations, there is less air above a given point, resulting in lower pressure.
  • Effects and Applications:
  • Weather Forecasting: Atmospheric pressure readings are crucial for weather predictions. Changes in atmospheric pressure can indicate different weather patterns.
  • Engineering and Design: Atmospheric pressure is a key consideration in the design of aircraft, spacecraft, and various mechanical systems that operate in different atmospheric conditions.
  • Physical Sciences: Understanding atmospheric pressure is essential in fields such as meteorology, aviation, and chemistry.
  • Units of Measurement:
  • Absolute Pressure: Measures the total pressure including atmospheric pressure. For example, 14.7 psi absolute includes the atmospheric pressure at sea level.
  • Gauge Pressure: Measures the pressure relative to atmospheric pressure. For example, a tire pressure gauge might read 30 psi gauge, which means 30 psi above the atmospheric pressure.
  • Variation Factors:
  • Temperature: Warmer air expands and becomes less dense, which can lower atmospheric pressure.
  • Humidity: Higher humidity reduces air density, which can also lower atmospheric pressure.
  • Weather Systems: Low and high-pressure systems influence weather conditions and can cause variations in atmospheric pressure.
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