Pressure measurement using a barometer is crucial for gathering data about the atmosphere. The pressure noted by the barometer uses the height of the mercury column to indicate the force exerted by air. The standard atmospheric pressure at sea level is defined as 760 millimeters (or 29.92 inches) of mercury. This precise measurement provides important insights into various scientific applications:
- Weather forecasting, where pressure changes can signal upcoming weather shifts.
- Determining altitude or elevation, as rising places experience lower pressure.
- Calculating the boiling points of different liquids, which alter with pressure.
Ensuring accuracy, though, means ensuring the barometer is free of contaminants that could skew readings, such as water droplets.