Broadening is due both to the natural width of the transition and to the velocity spread of the absorbing atoms along the line of sight.



be the normalized distribution of atoms with
velocity between v and 


= velocity of the cloud relative to the observer.
This full expression (1) is denoted as a ``Maxwell + damping wing'' or ``Voigtian'' profile in the program.
In the case of low column density (
1)
can be approximated to:
= NS



This simplified expression (2) is denoted as a ``Maxwellian'' profile in the
program.
Finally if the line of sight crosses N clouds then, the resulting optical depth is:

In cases where the source has a (cosmological) velocity.
Let z be the redshift of the source.
An absorption is measured in the spectrum at
=
corresponding to a rest wavelength
.
This yields for the redshift of the cloud:

The velocity of the cloud relative to the source is:


In practice the program computes the absorption profile in the cloud reference
frame
(
= 0) and shifts the result into the observer's rest frame
