REVEAL: A Global Full-Waveform Inversion Model

被引:2
|
作者
Thrastarson, Solvi [1 ]
van Herwaarden, Dirk-Philip [1 ]
Noe, Sebastian [1 ]
Schiller, Carl Josef [1 ]
Fichtner, Andreas [1 ]
机构
[1] Swiss Fed Inst Technol, Dept Earth Sci, Zurich, Switzerland
基金
欧盟地平线“2020”; 欧洲研究理事会;
关键词
SPECTRAL ELEMENT METHOD; SHEAR-VELOCITY MODEL; DISCONTINUOUS GALERKIN METHOD; UPPER-MANTLE STRUCTURE; EARTH STRUCTURE; MOMENT TENSORS; UNSTRUCTURED MESHES; ADJOINT TOMOGRAPHY; ELASTIC-WAVES; TRAVEL-TIME;
D O I
10.1785/0120230273
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present REVEAL, a global-scale, transversely isotropic full-waveform inversion model. REVEAL builds upon the earlier construction of the long-wavelength Earth (LOWE) model by lowering the minimum period from 100 to 33 s and by more than doubling the number of included earthquakes to 2366. In the course of 305 quasi-Newton iterations, REVEAL assimilated a total of 6,005,727 unique three-component waveforms. The inversion method rests on the combination of a stochastic mini -batch optimization and wavefield-adapted spectral-element meshes. Although the former naturally exploits redundancies in the data set, the latter reduces the cost of wavefield simulations by reducing the effective dimension of the numerical mesh. As a consequence, the average cost of an iteration in this inversion is only around 0.62% of an iteration that uses the complete data set with a standard cubed-sphere-type mesh. We calculated 3D synthetic seismograms using a graphics processing unit-accelerated spectral-element wave propagation solver, accommodating the effects of anelasticity, topography, bathymetry, ocean loading, and ellipticity. For a diverse range of global wavepaths, REVEAL predicts complete three-component seismograms at 33 s period that have not been included in the inversion. This generalization to unseen data suggests applications of REVEAL in event location and characterization, as well as in ground-motion modeling.
引用
收藏
页码:1392 / 1406
页数:15
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