Ambient Seismic Source Inversion in a Heterogeneous Earth: Theory and Application to the Earth's Hum

The sources of ambient seismic noise are extensively studied both to better understand their influence on ambient noise tomography and related techniques, and to infer constraints on their excitation mechanisms. Here we develop a gradient-based inversion method to infer the space-dependent and time-...

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Bibliographic Details
Main Authors: Ermert, Laura, Sager, Korbinian, Afanasiev, Michael, Boehm, Christian, Fichtner, Andreas
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2017
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/240647
https://doi.org/10.3929/ethz-b-000225762
Description
Summary:The sources of ambient seismic noise are extensively studied both to better understand their influence on ambient noise tomography and related techniques, and to infer constraints on their excitation mechanisms. Here we develop a gradient-based inversion method to infer the space-dependent and time-varying source power spectral density of the Earth's hum from cross correlations of continuous seismic data. The precomputation of wavefields using spectral elements allows us to account for both finite-frequency sensitivity and for three-dimensional Earth structure. Although similar methods have been proposed previously, they have not yet been applied to data to the best of our knowledge. We apply this method to image the seasonally varying sources of Earth's hum during North and South Hemisphere winter. The resulting models suggest that hum sources are localized, persistent features that occur at Pacific coasts or shelves and in the North Atlantic during North Hemisphere winter, as well as South Pacific coasts and several distinct locations in the Southern Ocean in South Hemisphere winter. The contribution of pelagic sources from the central North Pacific cannot be constrained. Besides improving the accuracy of noise source locations through the incorporation of finite-frequency effects and 3-D Earth structure, this method may be used in future cross-correlation waveform inversion studies to provide initial source models and source model updates. ISSN:2169-9313 ISSN:0148-0227 ISSN:2169-9356