Atmospheric pressure

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 (MSLP) is the atmospheric pressure at mean sea level. This is the atmospheric pressure normally given in weather reports via meteorologists on radio, television, and newspapers or on the Internet. The altimeter setting in aviation is an atmospheric pressure adjustment. Average sea-level pressure is . In aviation weather reports (METAR), QNH is transmitted around the world in hectopascals or millibars (1 hectopascal = 1 millibar). In the United States, Canada, and Japan altimeter setting is reported in inches of mercury (to two decimal places). 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; 998.7hPa is transmitted as 987; etc. A system transmitting the last three digits transmits the same code (800) for 1080.0 hPa as for 980.0 hPa. 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 centres 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 (terrain and oceans). It is directly proportional to the mass of air over that location. For numerical reasons, atmospheric models such as general circulation models (GCMs) 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 (MSL) in the International Standard Atmosphere (ISA) is 1,013.25 hPa, or 1 atmosphere (atm), or 29.92 inches of mercury. Pressure (P), mass (m), and acceleration due to gravity (g) are related by P = F/A = (m*g)/A, where A is the surface area. Atmospheric pressure is thus proportional to the weight per unit area of the atmospheric mass above that location. == Altitude variation ==

(Iceland), formed above the mountain by orographic lift 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. Pressure is proportional to temperature and inversely related to humidity, and both of these are necessary 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 (the barometric formula) relates atmospheric pressure p to altitude h: \begin{align} p &= p_0 \cdot \left(1 + \frac{L \cdot h}{T_0} \right)^{-\frac{g \cdot M}{R_0 \cdot L}} \\ &= p_0 \cdot \left(1 + \frac{g \cdot h}{c_\text{p} \cdot T_0} \right)^{-\frac{c_\text{p} \cdot M}{R_0}} \end{align} The values in these equations are: == Local variation ==

on 19 October 2005. The pressure in the eye of the storm was at the time the image was taken. Atmospheric pressure varies widely on Earth, and differences in pressure are important in studying weather and climate. Some variations in pressure are very regular. One important source of variation is atmospheric tides. Atmospheric tides are strongest in tropical zones, with an amplitude of a few hectopascals, and almost zero in polar areas. Tropical tidal variations in pressure consist principally of two superimposed harmonicsa circadian (24 h) cycle and a semi-circadian (12 h) cycle. == Records ==

The highest adjusted-to-sea level barometric pressure ever recorded on Earth above 750 meters was , measured in Tosontsengel, Mongolia on 19 December 2001. The highest adjusted-to-sea level barometric pressure ever recorded below 750 meters was at Agata, in Evenk Autonomous Okrug, Russia (66°53'N, 93°28'E, elevation: ), on 31 December 1968 of . The discrepancy is due to a problematic assumption (a standard lapse rate) associated with normalizing measurements of pressure at high elevations to standard sea level; at greater altitudes the conversion becomes progressively less precise, and for record purposes 750 m is the arbitrary threshold for adequate precision. A below-sea-level surface pressure record of was set on 21 February 1961. The lowest non-tornadic atmospheric pressure ever measured was , 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 the depth of water ==

One atmosphere () is also the pressure caused by the weight of a column of freshwater of approximately . Thus, a diver 10.3 m under water experiences a pressure of about 2 atmospheres (1 atm of air plus 1 atm of water). 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. (water column) gauge or w.g. (inches water) gauge. A typical gas-using residential appliance in the US is rated for a maximum of , 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 liquids ==

Pure water boils at at Earth's standard atmospheric pressure. The boiling point is the temperature at which the vapour pressure is equal to the atmospheric pressure around the liquid. Because of this, the boiling point of liquids 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. Conversely, if one wishes to evaporate a liquid at a lower temperature, for example in distillation, the atmospheric pressure may be lowered by using a vacuum pump, as in a rotary evaporator. == 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 reliable pressure measurement devices. In 1774, Nevil Maskelyne was confirming Newton's theory of gravitation at and on Schiehallion mountain in Scotland, and he needed to measure elevations on the mountain's sides accurately. This event is known as the Schiehallion experiment. William Roy, using barometric pressure, was able to confirm Maskelyne's height determinations; the agreement was within one meter (3.28 feet). This method became and continues to be useful for survey work and map making. == See also ==