A barometer is a scientific instrument used to measure atmospheric pressure. Atmospheric pressure is the force per unit area exerted on a surface by the weight of the air above that surface in the Earth's atmosphere. A barometer is an important tool for meteorologists as it helps in predicting short-term changes in the weather, particularly for forecasting storms.
There are two main types of barometers:
Barometers work based on the principle that as atmospheric pressure increases, the weight of the air above the barometer increases, causing the mercury level or the aneroid cell to respond accordingly. This change in the height of the mercury column or the movement of the aneroid cell is then used to determine the atmospheric pressure.
The main purpose of a barometer is to measure atmospheric pressure.
A mercury barometer works by using a column of mercury to measure atmospheric pressure. As the pressure changes, it causes the level of mercury in the column to rise or fall.
A mercury barometer uses a column of mercury, while an aneroid barometer uses a flexible metal box called an aneroid cell to measure atmospheric pressure.
A barometer is important for meteorologists because it helps in predicting short-term changes in the weather, particularly for forecasting storms.