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Misfit Functionals and Adjoint Sources

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Full Seismic Waveform Modelling and Inversion

Abstract

The early developments of full waveform inversion for 2D acoustic problems (e.g. Tarantola, 1984; Gauthier et al., 1986) were almost immediately followed by the recognition that the choice of a suitable misfit functional is crucial for a successful application to real data. In one of the first large-scale full waveform inversions, Crase et al. (1990) proposed a series of robust misfit measures that are comparatively insensitive to seismic noise. Their study was extended by Brossier et al. (2010). The L 2 distance between observed and synthetic seismograms is efficient for the detection of sharp material contrasts, but the recovery of long-wavelength Earth structure requires misfit functionals that explicitly extract phase information. In their pioneering work, Luo & Schuster (1991) therefore proposed to measure the cross-correlation time shift between observed and synthetic waveforms (Sect. 11.3). This idea was extended by van Leeuwen & Mulder (2010).

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Fichtner, A. (2011). Misfit Functionals and Adjoint Sources. In: Full Seismic Waveform Modelling and Inversion. Advances in Geophysical and Environmental Mechanics and Mathematics. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-15807-0_11

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