Description
The ISA mathematical model divides the atmosphere into layers with an assumed linear distribution of absolute temperature T against geopotential altitude h.^{[2]} The other two values (pressure P and density ρ) are computed by simultaneously solving the equations resulting from:
 the vertical pressure gradient resulting from hydrostatic balance, which relates the rate of change of pressure with geopotential altitude:
 ${\frac {dP}{dh}}=\rho g$, and
 $\ P=\rho R_{\rm {specific}}T$
at each geopotential altitude, where g is the standard acceleration of gravity, and R_{specific} is the specific gas constant for dry air.
Air density must be calculated in order to solve for the pressure, and is used in calculating dynamic pressure for moving vehicles. Dynamic viscosity is an empirical function of temperature, and kinematic viscosity is calculated by dividing dynamic viscosity by the density.
Thus the standard consists of a tabulation of values at various altitudes, plus some formulas by which those values were derived. To accommodate the lowest points on Earth, the model starts at a base geopotential altitude of 610 meters (2,000 ft) below sea level, with standard temperature set at 19 °C. With a temperature lapse rate of −6.5 °C (11.7 °F) per km (roughly −2 °C (3.6 °F) per 1,000 ft), the table interpolates to the standard mean sea level values of 15 °C (59 °F) temperature, 101,325 pascals (14.6959 psi) (1 atm) pressure, and a density of 1.2250 kilograms per cubic meter (0.07647 lb/cu ft). The tropospheric tabulation continues to 11,000 meters (36,089 ft), where the temperature has fallen to −56.5 °C (−69.7 °F), the pressure to 22,632 pascals (3.2825 psi), and the density to 0.3639 kilograms per cubic meter (0.02272 lb/cu ft). Between 11 km and 20 km, the temperature remains constant.^{[3]}^{[4]}
Layers in the ISA
Standard Atmosphere 1976
Layer

Level Name

Base Geopotential Altitude above MSL^{[5]} h (m)

Base Geometric Altitude above MSL^{[5]} z (m)

Lapse Rate ( °C/km)^{[a]}

Base Temperature T (°C)

Base Atmospheric Pressure p (Pa)

Base Atmospheric Density ρ (kg/m3)

0

Troposphere

610

611

+6.5

+19.0

108,900 (1.075 bar)

1.2985

1

Tropopause

11,000

11,019

0.0

−56.5

22,632

0.3639

2

Stratosphere

20,000

20,063

1.0

−56.5

5474.9

0.0880

3

Stratosphere

32,000

32,162

2.8

−44.5

868.02

0.0132

4

Stratopause

47,000

47,350

0.0

−2.5

110.91

0.0020

5

Mesosphere

51,000

51,413

+2.8

−2.5

66.939


6

Mesosphere

71,000

71,802

+2.0

−58.5

3.9564


7

Mesopause

84,852

86,000

—

−86.28

0.3734


 ^{a} lapse rate given per kilometer of geopotential altitude
In the above table, geopotential altitude is calculated from a mathematical model that adjusts the altitude to include the variation of gravity with height, while geometric altitude is the standard direct vertical distance above mean sea level.^{[2]} Note that the Lapse Rates cited in the table are given as °C per kilometer of geopotential altitude, not geometric altitude.
The ISA model is based on average conditions at mid latitudes, as determined by the ISO's TC 20/SC 6 technical committee. It has been revised from time to time since the middle of the 20th century.
Use at nonstandard day conditions
The ISA models a hypothetical standard day to allow a reproducible engineering reference for calculation and testing of engine and vehicle performance at various altitudes. It does not provide a rigorous meteorological model of actual atmospheric conditions (for example, changes in barometric pressure due to wind conditions). Neither does it account for humidity effects; air is assumed to be dry and clean and of constant composition. Humidity effects are accounted for in vehicle or engine analysis by adding water vapor to the thermodynamic state of the air after obtaining the pressure and density from the standard atmosphere model.
Nonstandard (hot or cold) days are modeled by adding a specified temperature delta to the standard temperature at altitude, but pressure, density, and viscosity are not recalculated at the resultant nonstandard temperature. (Thus the temperature effects on them are considered to be much less important than the effect of altitude.) Hot day, Cold day, Tropical, and Polar temperature profiles with altitude have been defined for use as performance references, such as United States Department of Defense MILSTD210C, and its successor MILHDBK310.^{[6]}