We here list the features added after the publication of arXiv:2207.06910.
Developed by Francesco Iacovelli and Michele Mancarella.
The TaylorF2_RestrictedPN
waveform can be extended up to the Kerr ISCO of the remnant BH (rather than assuming it to be a Schwarzschild BH), computed as in arXiv:2108.05861 (see Appendix C in particular), with the fits from arXiv:1605.01938. This can be done thanks to the which_ISCO
flag as follows:
mywf = waveforms.TaylorF2_RestrictedPN(which_ISCO='Kerr')
We added a function to compute the overlap between two waveforms on two sets of event parameters. This is defined as
with
This can be computed both from a GWSignal
object or a DetNet
object as
overlap = myNet.WFOverlap(WF1, WF2, Params1, Params2)
with WF1
and WF2
being two waveform objects and Params1
and Params2
being tow dictionaries containing the parameters of the events (as the standard inputs of the SNR
or FisherMatr
functions). This will return an array
with the overlaps of the two waveforms on the two sets of parameters, with the overlap being 1 in case of perfect match.
The TaylorF2_RestrictedPN
waveform can include the spin-induced quadrupole coefficient as a function the dimensionless tidal deformability, computed as in Eq. (15) of arXiv:1608.02582 with coeffs from third row of Table I. This can be done thanks to the use_QuadMonTid
flag as follows:
mywf = waveforms.TaylorF2_RestrictedPN(is_tidal=True, use_QuadMonTid=True)
Notice the is_tidal
flag has to be set to True
for this to work (the spin-induced quadrupole coefficient for a BH is 1).
We added a wrapper to use the TEOBResumSPA
waveform model of the TEOBResumS
family, available on Bitbucket here, see arXiv:2104.07533, arXiv:2012.00027, arXiv:2001.09082, arXiv:1904.09550, arXiv:1806.01772, arXiv:1506.08457, arXiv:1406.6913. This is a frequency-domain waveform model which can be used both for BBH, BNS and NSBH binaries, including contribution of higher-order modes and tidal effects. It can be used simply as
mywf = waveforms.TEOBResumSPA_WF()
The flag is_tidal=True
can be used if willing to include tidal effects, and the argument modes
can be used to specify which modes to include in the analysis. It has to be a list of 2-elements lists containig the l and m of the desired modes (in this order), as e.g.
mywf = waveforms.TEOBResumSPA_WF(modes=[[2,1], [2,2]])
In this case the waveform includes the dominant quadrupole (l=2, m=2) mode plus the sub-dominant (l=2, m=1) mode.
The default is to include all the modes up to l=4, i.e. modes=[[2,1], [2,2], [3,1], [3,2], [3,3], [4,1], [4,2], [4,3], [4,4]]
The implementation matches the one used in the examples available here.
When using this waveform model, derivatives are computed using numerical differentiation (finite differences).
To use this model in the calculate_forecasts_from_catalog.py
script, set --wf_model='TEOBResumSPA'
for the BBH version, or --wf_model='TEOBResumSPA_tidal'
to include tidal effects.
We added a function to compute the relative orientation of two detectors with respect to the great circle that joins them. This can be used as
angle = utils.ang_btw_dets_GC(det_1, det_2)
with det_1
and det_2
being two dictionaries containing the latitude ('lat'
), longitude ('long'
) and orientation (xax
) of the two detectors (in degrees), as the ones given in the detectors
dictionary present in the gwfastGlobals.py
module.
To compute their great circle distance we added the function
dist_GC = utils.dist_btw_dets_GC(det_1, det_2)
whose output is given in kilometers.
We further added a function to compute the great circle chord length between two detectors
dist_GC = utils.dist_btw_dets_Chord(det_1, det_2)
whose output is again given in kilometers.