Multitaper Misfit
Warning
Please refer to [Laske1996] for a more rigorous mathematical derivation of this misfit function.
The misfit \(\chi_P(\mathbf{m})\) measures frequency-dependent phase differences estimated with multitaper methods. For a given Earth model \(\mathbf{m}\) and a single receiver, \(\chi_P(\mathbf{m})\) is given by
\(\tau^\mathbf{d}(w)\) is the frequency-dependent phase measurement of the observed data; \(\tau^\mathbf{s}(w, \mathbf{m})\) the frequency-dependent phase measurement of the synthetic data.
The function \(W_P(w)\) denotes frequency-domain taper corresponding to the frequency range over which the measurements are assumed reliable. \(\sigma_P(w)\) is associated with the traveltime uncertainty introduced in making measurements, which can be estimated with cross-correlation method, or Jackknife multitaper approach.
The adjoint source for the same receiver is given by
in which \(h_k(t)\) is one (the \(k\) th) of multi-tapers.
Usage
adjsrc_type = "multitaper"
The following code snippet illustrates the basic usage of the cross correlation traveltime misfit function. See the corresponding Config object for additional configuration parameters.
import pyadjoint
obs, syn = pyadjoint.get_example_data()
obs = obs.select(component="Z")[0]
syn = syn.select(component="Z")[0]
config = pyadjoint.get_config(adjsrc_type="multitaper", min_period=20.,
max_period=100.)
adj_src = pyadjoint.calculate_adjoint_source(config=config,
observed=obs, synthetic=syn,
windows=[(800., 900.)]
)