Atmospheric pressure


Atmospheric pressure, also known as barometric pressure, is the pressure within the atmosphere of Earth. The standard atmosphere is a unit of pressure defined as, which is equivalent to 760mm Hg, 29.9212inchesHg, or 14.696psi. The atm unit is roughly equivalent to the mean sea-level atmospheric pressure on Earth, that is, the Earth's atmospheric pressure at sea level is approximately 1 atm.
In most circumstances, atmospheric pressure is closely approximated by the hydrostatic pressure caused by the weight of air above the measurement point. As elevation increases, there is less overlying atmospheric mass, so that atmospheric pressure decreases with increasing elevation. Pressure measures force per unit area, with SI units of Pascals. On average, a column of air with a cross-sectional area of 1 square centimetre, measured from mean sea level to the top of Earth's atmosphere, has a mass of about 1.03 kilogram and exerts a force or "weight" of about 10.1 newtons, resulting in a pressure of 10.1 N/cm2 or 101kN/m2. A column of air with a cross-sectional area of 1in2 would have a weight of about 14.7lbf, resulting in a pressure of 14.7lbf/in2.

Mechanism

Atmospheric pressure is caused by the gravitational attraction of the planet on the atmospheric gases above the surface, and is a function of the mass of the planet, the radius of the surface, and the amount and composition of the gases and their vertical distribution in the atmosphere. It is modified by the planetary rotation and local effects such as wind velocity, density variations due to temperature and variations in composition.

Mean sea-level pressure

The mean sea-level pressure is the atmospheric pressure at mean sea level. This is the atmospheric pressure normally given in weather reports on radio, television, and newspapers or on the Internet. When barometers in the home are set to match the local weather reports, they measure pressure adjusted to sea level, not the actual local atmospheric pressure.
The altimeter setting in aviation is an atmospheric pressure adjustment.
Average sea-level pressure is. In aviation, weather reports, QNH is transmitted around the world in millibars or hectopascals, except in the United States, Canada, and Colombia where it is reported in inches of mercury. The United States and Canada also report sea-level pressure SLP, which is adjusted to sea level by a different method, in the remarks section, not in the internationally transmitted part of the code, in hectopascals or millibars. However, in Canada's public weather reports, sea level pressure is instead reported in kilopascals.
In the US weather code remarks, three digits are all that are transmitted; decimal points and the one or two most significant digits are omitted: is transmitted as 132; is transmitted as 000; 998.7mbar is transmitted as 987; etc. The highest sea-level pressure on Earth occurs in Siberia, where the Siberian High often attains a sea-level pressure above, with record highs close to. The lowest measurable sea-level pressure is found at the centers of tropical cyclones and tornadoes, with a record low of.

Surface pressure

Surface pressure is the atmospheric pressure at a location on Earth's surface. It is directly proportional to the mass of air over that location.
For numerical reasons, atmospheric models such as general circulation models usually predict the nondimensional logarithm of surface pressure.
The average value of surface pressure on Earth is 985 hPa. This is in contrast to mean sea-level pressure, which involves the extrapolation of pressure to sea-level for locations above or below sea-level. The average pressure at mean sea-level in the International Standard Atmosphere is 1013.25 hPa, or 1 atmosphere, or 29.92 inches of mercury.
Pressure, mass, and the acceleration due to gravity, are related by P = F/A = /A, where A is surface area. Atmospheric pressure is thus proportional to the weight per unit area of the atmospheric mass above that location.

Altitude variation

Pressure on Earth varies with the altitude of the surface; so air pressure on mountains is usually lower than air pressure at sea level. Pressure varies smoothly from the Earth's surface to the top of the mesosphere. Although the pressure changes with the weather, NASA has averaged the conditions for all parts of the earth year-round. As altitude increases, atmospheric pressure decreases. One can calculate the atmospheric pressure at a given altitude. Temperature and humidity also affect the atmospheric pressure, and it is necessary to know these to compute an accurate figure. The graph was developed for a temperature of 15 °C and a relative humidity of 0%.
At low altitudes above sea level, the pressure decreases by about for every 100 metres. For higher altitudes within the troposphere, the following equation relates atmospheric pressure p to altitude h:
where the constant parameters are as described below:
ParameterDescriptionValue
p0Sea level standard atmospheric pressure101325Pa
LTemperature lapse rate, = g/cp for dry air~ 0.00976K/m
cpConstant-pressure specific heat1004.68506J/
T0Sea level standard temperature288.16K
gEarth-surface gravitational acceleration9.80665m/s2
MMolar mass of dry air0.02896968kg/mol
R0Universal gas constant8.314462618J/

Local variation

Atmospheric pressure varies widely on Earth, and these changes are important in studying weather and climate. See pressure system for the effects of air pressure variations on weather.
Atmospheric pressure shows a diurnal or semidiurnal cycle caused by global atmospheric tides. This effect is strongest in tropical zones, with an amplitude of a few millibars, and almost zero in polar areas. These variations have two superimposed cycles, a circadian cycle and semi-circadian cycle.

Records

The highest adjusted-to-sea level barometric pressure ever recorded on Earth was measured in Tosontsengel, Mongolia on 19 December 2001. The highest adjusted-to-sea level barometric pressure ever recorded was at Agata in Evenk Autonomous Okrug, Russia on 31 December 1968 of. The discrimination is due to the problematic assumptions associated with reduction of sea level from high elevations.
The Dead Sea, the lowest place on Earth at below sea level, has a correspondingly high typical atmospheric pressure of 1065hPa. A below-sea-level surface pressure record of was set on 21 February 1961.
The lowest non-tornadic atmospheric pressure ever measured was 870 hPa, set on 12 October 1979, during Typhoon Tip in the western Pacific Ocean. The measurement was based on an instrumental observation made from a reconnaissance aircraft.

Measurement based on depth of water

One atmosphere is also the pressure caused by the weight of a column of fresh water of approximately 10.3 m. Thus, a diver 10.3 m underwater experiences a pressure of about 2 atmospheres. Conversely, 10.3 m is the maximum height to which water can be raised using suction under standard atmospheric conditions.
Low pressures such as natural gas lines are sometimes specified in inches of water, typically written as w.c. gauge or w.g.. A typical gas-using residential appliance in the US is rated for a maximum of 1/2 psi, which is approximately 14 w.g.. Similar metric units with a wide variety of names and notation based on millimetres, centimetres or metres are now less commonly used.

Boiling point of water

Pure water boils at at earth's standard atmospheric pressure. The boiling point is the temperature at which the vapor pressure is equal to the atmospheric pressure around the water. Because of this, the boiling point of water is lower at lower pressure and higher at higher pressure. Cooking at high elevations, therefore, requires adjustments to recipes or pressure cooking. A rough approximation of elevation can be obtained by measuring the temperature at which water boils; in the mid-19th century, this method was used by explorers.

Measurement and maps

An important application of the knowledge that atmospheric pressure varies directly with altitude was in determining the height of hills and mountains thanks to the availability of reliable pressure measurement devices. In 1774, Maskelyne was confirming Newton's theory of gravitation at and on Schiehallion mountain in Scotland, and he needed to accurately measure elevations on the mountain's sides. William Roy, using barometric pressure, was able to confirm Maskelyne's height determinations, the agreement being to within one meter. This method became and continues to be useful for survey work and map making.

Experiments

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