ISA Atmosphere Model
Implement International Standard Atmosphere (ISA)
Libraries:
Aerospace Blockset /
Environment /
Atmosphere
Alternative Configurations of ISA Atmosphere Model Block:
Lapse Rate Model
Description
The ISA Atmosphere Model block implements the mathematical representation of the International Standard Atmosphere (ISA) values for ambient temperature, pressure, density, and speed of sound for the input geopotential altitude.
The ISA Atmosphere Model and Lapse Rate Model blocks are alternative configurations of the same block.
The ISA Atmosphere Model block has these implementations:
ISA Atmosphere Model — The default ISA model implements the mathematical representation of the ISA values for ambient temperature, pressure, density, and speed of sound for the input geopotential altitude between sea level (0 m) and tropopause (20000 m).
Lapse Rate Model — The lapse rate model implements the mathematical representation of the lapse rate atmospheric equations for ambient temperature, pressure, density, and speed of sound for the input geopotential altitude. To convert from the ISA implementation to the Lapse Rate implementation, select the Change atmospheric parameters parameter. You can customize this atmospheric model by specifying atmospheric properties.
To implement the mathematical representation of the ISA values for ambient temperature, pressure, density, and speed of sound for the input geopotential altitude between -5000 m and mesopause (84852 m), select the Use extended ISA model parameter.
The ISA Atmosphere Model block icon displays the input and output port labels in metric units.
Limitations
In the default model, the block limits the implementation to the geopotential altitude of 0 m (minimum) and 20000 m (maximum). In the extended model, the limits are -5000 meters (minimum) and 84852 meters (maximum). The limits are inclusive.
Density and speed of sound are calculated using a perfect gas relationship.
Ports
Input
Output
Parameters
Alternative Configurations
Algorithms
The dynamic viscosity is computed using [1]:
The kinematic viscosity is computed using [1]:
where:
β — A constant dependent on the reference temperature and dynamic viscosity.
T — Kelvin kinetic temperature.
S — Sutherland constant.
ρ — Mass density of air.
References
[1] U.S. Standard Atmosphere., Washington, D.C.: U.S. Government Printing Office, 1976.