What is Atmospheric Pressure and How is it Measured?
Atmospheric pressure affects your everyday life whether you are aware of it or not. Weather patterns and forecasts around the world are affected by atmospheric pressure, but many don’t actually know what it actually is. And once you’ve learned the basics of atmospheric pressure, you can better understand how to measure it. Keep reading to learn more.
What is Atmospheric Pressure?
Essentially, atmospheric pressure is the force exerted at any given point on the Earth’s surface by the weight of the air above that point. In short: the air that surrounds the Earth creates atmospheric pressure and this pressure is determined by the collective weight of air molecules. Air molecules at higher altitudes have fewer molecules pressing down on them from above and therefore experience lower pressure, while lower molecules have more force or pressure exerted on them by molecules piled on top of them and are more tightly packed together.
When you go up into the mountains or fly high in an airplane, the air is thinner and the pressure is lower. The air pressure at sea level at a temperature of 59°F (15°C) is equal to one atmosphere (Atm), and this is the baseline reading for determining relative pressure.
Atmospheric pressure is also known as barometric pressure because it is measured using a barometer. A rising barometer indicates increasing atmospheric pressure and a falling barometer indicates decreasing atmospheric pressure.
How Is Barometric Pressure Measured?
The standard unit for measuring barometric pressure is called an atmosphere (atm). In relation to the English system of measurement, one atmosphere (atm) equals 29.9213 inches of mercury (inHg). In both millibars (mb) and hectopascal (hPa), the standard pressure at sea level is 1013.25 mb or hPa. Other conversions include:
- 1 atm = 101,325 pascals (Pa)
- 1 atm = 1,013.25 hectopascals (hPa)
- 1 atm = 760 millimeters of mercury (mmHg)
- 1 atm = 1,013.25 millibars (mbar)
What Causes Changes in Atmospheric Pressure?
Changes in air pressure are caused by differences in air temperature above the earth, and the temperature of an air mass is determined by its location. For example, air masses above oceans are typically cooler than air masses above continents. Air temperature differences create wind and cause pressure systems to develop. The wind moves pressure systems and these systems tend to change as they pass over mountains, oceans, and other areas.
17th-century French scientist and philosopher Blaise Pascal (1623–1662) discovered that air pressure decreases with height and that pressure-changes at ground level can be attributed to the daily weather. These discoveries are used to predict the weather today.
Often, weather forecasters refer to high- or low-pressure areas moving toward particular regions in order to describe predicted conditions for those areas. As air rises in low-pressure systems, it cools and often condenses into clouds and precipitation, resulting in storms. In high-pressure systems, the air sinks toward the Earth and warms upward, leading to dry and fair weather.
Why Does Atmospheric Pressure Change With Altitude?
Simply put, when altitude increases, the amount of gas molecules in the atmosphere decreases (air becomes less dense), hence the term “thin air” which is used most commonly used in climbing, hiking, and mountaineering.
How Pressure Changes Affect the Weather
In general, a barometer can let you know if your immediate future will see clearing or stormy skies, or little change at all, based only on atmospheric pressure.
Here are a few examples of how to interpret barometric readings:
- When the air is dry, cool, and pleasant, the barometer reading rises.
- In general, a rising barometer means improving weather.
- In general, a falling barometer means worsening weather.
- When atmospheric pressure drops suddenly, this usually indicates that a storm is on its way.
- When atmospheric pressure remains steady, there will likely be no immediate change in the weather.
How Do You Measure Atmospheric Pressure with a Barometer?
Reading a barometer is simple if you know what different atmospheric pressure values indicate. To understand your barometer and how atmospheric pressure is changing, interpret readings as follows (pay attention to units).
Measuring High Pressure (Anticyclone)
A barometric reading over 30.20 inHg is generally considered high, and high pressure is associated with clear skies and calm weather.
If the reading is over 30.20 inHg (102268.9 Pa or 1022.689 mb):
- Rising or steady pressure means continued fair weather.
- Slowly falling pressure means fair weather.
- Rapidly falling pressure means cloudy and warmer conditions.
Measuring Normal Pressure
A barometric reading in the range of 29.80 and 30.20 inHg can be considered normal, and normal pressure is associated with steady weather.
If the reading falls between 29.80 and 30.20 inHg (100914.4–102268.9 Pa or 1022.689–1009.144 mb):
- Rising or steady pressure means present conditions will continue.
- Slowly falling pressure means little change in the weather.
- Rapidly falling pressure means that rain is likely, or snow if it is cold enough.
Measuring Low Pressure (Depression)
A barometric reading below 29.80 inHg is generally considered low, and low pressure is associated with warm air and rainstorms.
If the reading is under 29.80 inHg (100914.4 Pa or 1009.144 mb):
- Rising or steady pressure indicates clearing and cooler weather.
- Slowly falling pressure indicates rain.
- Rapidly falling pressure indicates a storm is coming.
If you are interested in measuring atmospheric pressure right at your own home, take a look through Maximum’s wide variety of barometers. And if you have a question about your barometer or how to use it, feel free to contact us today.