How to make a barometer

You may ask
how to make a barometer
quickly and easily. This device should work and making a barometer will help demonstrate the principles outlined below. To make your own barometer,
find
a jar, metric ruler, straw, tape and some gum. Then come back here. - First of all, tape the ruler to the inside of the jar so that you can read the numbers and it stays standing upright.
- Tape your straw to the ruler, but don't cover the numbers. Leave a small space between the end of the straw and the bottom of the jar.
- Chew your gum for awhile.
- Put some water in the jar - half full should do.
- Suck up a little water into the straw, but not all the way to your mouth. Then plug the top end of the straw with your gum. Make a good seal. This may take a little practice.
- Make a tick mark to remember where the water level is in the straw. Use a permanent marker.
- Wait and watch. The water level will change up and down. Moving up means higher
atmospheric pressure.
- How to make a barometer work: to calibrate, compare the movements in millimetres with the changes in reported
barometric pressure.
Determine how many observed pressure units, either kiloPascals or hundredths of an inch of mercury each millimeter on the ruler represents.
For best results, use your barometer indoors where the temperature remains almost constant.
Here are a few other barometer designs for the kids to try.

Make a barometer
- using an air balloon.
How to make a barometer
- with a can and a pin.
How does a barometer work?
The air pressure on the surface of the water in the jar in our simple example causes it to push upward on the water in the straw. That's why increasing the ambient pressure causes the column to go up. The mass of
air
above the water inside the straw does not change, but the increased pressure causes it to occupy a smaller space, provided the
temperature
does not change. The whole system seems to know how to make a barometer respond. One of Galileo's students, Evangelista Torricelli, wrote We live submerged at the bottom of an ocean of elementary air, which is known by incontestable experiments to have weight. This has become a famous quotation in meteorology. Barometers have been developed to help us determine that weight. Traditional barometers come in two types: Liquid barometers - someone figured out how to make a barometer with a vertical tube containing either water or mercury. If it has mercury, which is far more common, its height changes from around two to nearly three feet at ground level when the atmospheric pressure changes. How often does that happen? Every day, but not by a lot, usually. When people, usually American citizens and pilots, say that the pressure is 29 inches or some number close to that, they are talking about mercury. Most often, this is the height the mercury column would be if "corrected to sea level". Mathematically adjusted to give the
correct pressure
if the elevation were equal to zero.
What does elevation have to do with it? The air pressure drops off quickly as you climb uphill and this effect cannot be ignored when interpreting data.
Aneroid barometers - a
sealed container
cannot let air escape. When you have one of these with flexible walls, the walls move when the air pressure outside changes. And we can measure how much they move. How to make a barometer improve aviation safety? Airplanes use an aneroid barometer to help pilots figure out how high they are above the ground. They call this
device
an altimeter. Have fun with your barometer experiments.
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