Theory
The attenuation coefficient (Ambient air temperature) requires the molar concentration of water vapour . The program derives it from the relative humidity, the saturation vapour pressure over liquid water at the air temperature, and the ambient pressure, equations (1) and (2) (ISO 9613-1 Annex B).
The absorption does not vary monotonically with humidity: the humidity shifts the relaxation frequencies, and with them the frequency range in which each relaxation process absorbs most.
Equations
| where | meaning | unit |
|---|---|---|
| Molar concentration of water vapour | % | |
| Relative humidity (this setting) | % | |
| Saturation vapour pressure | kPa | |
| Ambient pressure | kPa | |
| Reference pressure, 101.325 | kPa | |
| Air temperature | K | |
| Triple-point isotherm temperature, 273.16 | K |
Default and rule
- Default
- 70 %
- Rule
70 %. This is the program's default, chosen within the tabulated range of 10-100 %; it is not taken from a standard.
- Source
ISO 9613-1 Annex B. The conversion is verified through the attenuation coefficients against tabulated values (see Ambient air temperature).
Valid range 10 to 100 %
Values
10 to 100 %.