millibar (mbar) to standard atmospheres (atm) conversion

What is millibar?

The millibar (mbar) is a unit of pressure commonly used in meteorology to measure atmospheric pressure. Understanding millibars helps in interpreting weather patterns and forecasts. Below is an overview of millibars, their relation to other units, and their significance.

Definition of Millibar

A millibar is defined as 100 Pascals (Pa), where a Pascal is the SI unit of pressure (force per unit area). The prefix "milli-" indicates one-thousandth, so:

$$1 \text{ mbar} = 100 \text{ Pa} = 1 \text{ hPa}$$

Another unit of pressure is standard atmosphere (atm)

$$1 \text{ atm} = 1013.25 \text{ mbar}$$

Formation and History

The term "bar" comes from the Greek word "báros," meaning weight. The bar was introduced by the British physicist Napier Shaw in 1909, and the millibar soon followed as a more practical unit for meteorology because typical atmospheric pressures on Earth are close to 1000 mbar.

Relation to Other Units

• Pascal (Pa): The SI unit of pressure. $1 \text{ mbar} = 100 \text{ Pa}$.
• Hectopascal (hPa): $1 \text{ hPa} = 1 \text{ mbar}$. Hectopascals are numerically equivalent to millibars and are commonly used in aviation.
• Atmosphere (atm): Standard atmospheric pressure at sea level is approximately $1013.25 \text{ mbar}$.
• Inches of Mercury (inHg): Commonly used in aviation in the United States. $1 \text{ mbar} \approx 0.02953 \text{ inHg}$.

Significance in Meteorology

Atmospheric pressure is a critical factor in weather forecasting. Here's how millibars are used:

• Weather Maps: Isobars (lines of equal pressure) on weather maps are often labeled in millibars, showing high and low-pressure systems.
• High-Pressure Systems: Associated with stable weather conditions, typically ranging from 1015 mbar to 1035 mbar or higher.
• Low-Pressure Systems: Associated with unsettled weather, such as storms and rain, typically ranging from 980 mbar to 1000 mbar or lower.
• Storm Intensity: The central pressure of a hurricane or cyclone is measured in millibars; lower pressures indicate stronger storms. For example, Hurricane Wilma in 2005 had a record low central pressure of 882 mbar.
• Aviation: Altitude is determined by measuring atmospheric pressure

Real-World Examples

• Standard Sea Level Pressure: The standard atmospheric pressure at sea level is approximately $1013.25 \text{ mbar}$.
• Hurricane Central Pressure: Intense hurricanes can have central pressures below $950 \text{ mbar}$. For example, Hurricane Katrina (2005) had a minimum central pressure of around $902 \text{ mbar}$.
• Mount Everest Summit Pressure: The atmospheric pressure at the summit of Mount Everest is roughly $330 \text{ mbar}$.
• Typical House Pressure: The pressure inside buildings is near $1013.25 \text{ mbar}$.

Interesting Facts and Associations

• Torricelli's Experiment: Evangelista Torricelli, an Italian physicist, invented the barometer in the 17th century, paving the way for accurate pressure measurement. Though he didn't use millibars (as the unit wasn't invented yet), his work laid the foundation for understanding atmospheric pressure. Learn more at Britannica.
• Beaufort Scale: While the Beaufort scale primarily measures wind speed, it indirectly relates to pressure gradients. Steeper pressure gradients (indicated by closely spaced isobars) typically result in stronger winds. More information is on the National Weather Service.

What is the standard atmosphere?

The standard atmosphere (atm) is a unit of pressure defined as a fixed reference value close to the average atmospheric pressure at sea level. It is widely used in chemistry, physics, engineering, and diving to express pressures relative to typical sea-level conditions.

Definition

The standard atmosphere is defined exactly as 101,325 pascals:

$$1\ \text{atm} = 101325\ \text{Pa}$$

This is equivalent to 1013.25 hectopascals (millibars), 760 millimeters of mercury (torr), and about 14.6959 pounds per square inch. The value was fixed by the 10th General Conference on Weights and Measures (CGPM) in 1954.

Origin and History

Early pressure measurement grew from Evangelista Torricelli's 1643 barometer experiments, which showed the atmosphere supports a mercury column about 760 mm high. The "atmosphere" became a convenient reference for a whole unit of ambient pressure. In 1954 the CGPM adopted the exact value 101,325 Pa, based on a 760 mm mercury column at 0 °C under standard gravity, to remove the temperature and location dependence of earlier definitions.

Law and Notable Facts

The standard atmosphere is accepted for use with the SI but is not an SI unit; the SI unit of pressure is the pascal. IUPAC now recommends the bar (100,000 Pa) rather than the atmosphere as the standard pressure for reporting thermodynamic data, though "atm" remains common. Note that the technical atmosphere (at) is a different unit equal to 98,066.5 Pa.

Real-World Examples and Conversions

• Average sea-level air pressure is very close to 1 atm (101.325 kPa).
• Ocean pressure increases by roughly 1 atm for every 10 meters of seawater depth, so a diver at 30 m experiences about 4 atm total.
• A typical car tire inflated to 32 psi holds about 2.2 atm of gauge pressure.
• The pressure inside a champagne bottle is roughly 6 atm (about 608 kPa).