Pressure and Altitude
Atmospheric pressure, sometimes referred to as barometric pressure, is a measure the total weight (or mass) of the atmosphere. It decreases with elevation and varies with time due to the passage of high- and low-pressure systems and other atmospheric phenomenon. Pressure was once measured using a device known as a Torricellian barometer, which was invented by Evangelista Torricelli in the 1600s. As illustrated below, a tube with a sealed end was filled with mercury and placed upside down in a bowl filled with mercury. The pressure of the atmosphere thus affects the mercury in the bowl, but not the tube. As a result, the mercury in the tube would rise until the weight per unit area of the mercury in the tube equaled the weight per unit area of the atmosphere and mercury out of the tube. Source: https://www.explainthatstuff.com/barometers.html . Mercury is of course poisonous, but had the advantage of being very dense. At sea level, the mercury ...