3.1. Reverberation Mapping Assumptions
There are a number of simplifying assumptions that we can now make:
![]() | (17) |
The time it takes a Lyman
photon to diffuse outward from
the Strömgren depth is about 20 times the direct light-travel time
35,
![]() | (18) |
We also need to carry out our reverberation-mapping experiment on a time scale short enough that the structure of the BLR can be assumed to be stable. The dynamical, or cloud-crossing, time scale for the BLR is typically
![]() | (19) |
where VFWHM is the Doppler width of the broad line for
which the response time =
r/c has been measured.
Any reverberation-mapping experiment has to be short relative
to the crossing time or the structural information might be
washed out by cloud motions.