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Barometric formula
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== Pressure equations == {{see also|Atmospheric pressure}} [[File:Pressure air.svg|thumb|300px|Pressure as a function of the height above the sea level]] There are two equations for computing pressure as a function of height. The first equation is applicable to the atmospheric layers in which the temperature is assumed to vary with altitude at a non null [[lapse rate]] of <math>L_b</math>: {{anchor|Non-zero lapse rate}} <math display="block">P = P_{b} \left[ 1 - \frac{L_{M,b}}{T_{M,b}} (h - h_{b})\right]^{\frac{g_{0}' M_{0}}{R^{*} L_{M,b}}}</math> The second equation is applicable to the atmospheric layers in which the temperature is assumed not to vary{{cn|date=August 2023}} with altitude ([[lapse rate]] is null): {{anchor|Zero lapse rate}} <math display="block">P = P_b \exp \left[\frac{-g_0 M \left(h-h_b\right)}{R^* {T_{M,b}}}\right]</math> where: *<math>P_b</math> = reference pressure *<math>T_{M,b}</math> = reference temperature ([[kelvin|K]]) *<math>L_{M,b}</math> = temperature lapse rate (K/m) in [[International Standard Atmosphere|ISA]] *<math>h</math> = [[geopotential height]] at which pressure is calculated (m) *<math>h_b</math> = geopotential height of reference level ''b'' (meters; e.g., ''h<sub>b</sub>'' = 11 000 m) *<math>R^*</math> = [[universal gas constant]]: 8.3144598 J/(mol路K) *<math>g_0</math> = [[standard gravity|gravitational acceleration]]: 9.80665 m/s<sup>2</sup> *<math>M</math> = molar mass of Earth's air: 0.0289644 kg/mol Or converted to [[imperial units]]:<ref name="conversion">Mechtly, E. A., 1973: ''[https://ntrs.nasa.gov/api/citations/19730018242/downloads/19730018242.pdf The International System of Units, Physical Constants and Conversion Factors]''. NASA SP-7012, Second Revision, National Aeronautics and Space Administration, Washington, D.C.</ref> *<math>P_b</math> = reference pressure *<math>T_{M,b}</math> = reference temperature ([[kelvin|K]]) *<math>L_{M,b}</math> = temperature lapse rate (K/ft) in [[International Standard Atmosphere|ISA]] *<math>h</math> = height at which pressure is calculated (ft) *<math>h_b</math> = height of reference level ''b'' (feet; e.g., ''h<sub>b</sub>'' = 36,089 ft) *<math>R^*</math> = [[universal gas constant]]; using feet, kelvins, and (SI) [[mole (unit)|moles]]: {{val|8.9494596e4|u=lb路ft<sup>2</sup>/(lb-mol路K路s<sup>2</sup>)}} *<math>g_0</math> = [[standard gravity|gravitational acceleration]]: 32.17405 ft/s<sup>2</sup> *<math>M</math> = molar mass of Earth's air: 28.9644 lb/lb-mol The value of subscript ''b'' ranges from 0 to 6 in accordance with each of seven successive layers of the atmosphere shown in the table below. In these equations, ''g''<sub>0</sub>, ''M'' and ''R''<sup>*</sup> are each single-valued constants, while ''P'', ''L,'' ''T,'' and ''h'' are multivalued constants in accordance with the table below. The values used for ''M'', ''g''<sub>0</sub>, and ''R''<sup>*</sup> are in accordance with the [[U.S. Standard Atmosphere]], 1976, and the value for ''R''<sup>*</sup> in particular does not agree with standard values for this constant.<ref name="USSA1976">[https://www.ngdc.noaa.gov/stp/space-weather/online-publications/miscellaneous/us-standard-atmosphere-1976/us-standard-atmosphere_st76-1562_noaa.pdf U.S. Standard Atmosphere], 1976, U.S. Government Printing Office, Washington, D.C., 1976. (Linked file is 17 Mb)</ref> The reference value for ''P<sub>b</sub>'' for ''b'' = 0 is the defined sea level value, ''P''<sub>0</sub> = 101 325 [[pascal (unit)|Pa]] or 29.92126 inHg. Values of ''P<sub>b</sub>'' of ''b'' = 1 through ''b'' = 6 are obtained from the application of the appropriate member of the pair equations 1 and 2 for the case when ''h'' = ''h''<sub>''b''+1</sub>.<ref name=USSA1976/> {| class="wikitable" style="text-align: center" |- ! rowspan="2"|Subscript ''b'' ! colspan="2"|Geopotential height above MSL (h) ! colspan="2"|Static pressure ! rowspan="2"|Standard temperature<br> (K) ! colspan="2"|Temperature lapse rate ! rowspan="2"|Exponent <br> g0 M / R L |- ! (m) !! (ft)!! (Pa) !! (inHg) !! (K/m) !! (K/ft) |- | 0 || 0 || 0 || 101 325.00 || 29.92126 || 288.15 || 0.0065 || 0.0019812 || 5.25588 |- | 1 || 11聽000 || 36,089 || 22 632.10 || 6.683245 || 216.65 || 0.0 || 0.0 || — |- | 2 || 20聽000 || 65,617 || 5474.89 || 1.616734 || 216.65 || -0.001 || -0.0003048 || -34.1626 |- | 3 || 32聽000 || 104,987 || 868.02 || 0.2563258 || 228.65 || -0.0028 || -0.00085344 || -12.2009 |- | 4 || 47聽000 || 154,199 || 110.91 || 0.0327506 || 270.65 || 0.0 || 0.0 || — |- | 5 || 51聽000 || 167,323 || 66.94 || 0.01976704 || 270.65 || 0.0028 || 0.00085344 || 12.2009 |- | 6 || 71聽000 || 232,940 || 3.96 || 0.00116833 || 214.65 || 0.002 || 0.0006096 || 17.0813 |}
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