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Full Waveform Inversion Based on an Asymptotic Solution of Helmholtz Equation

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Author
Protasov, Maxim
Gadylshin, Kirill
Neklyudov, Dmitry
Klimeš, LuděkORCiD Profile - 0000-0003-2991-4036WoS Profile - F-7058-2019Scopus Profile - 57193985220

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Publication date
2023
Published in
Geosciences (Switzerland)
Volume / Issue
13 (1)
ISBN / ISSN
ISSN: 2076-3263
Funding Information
UK/COOP/COOP
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  • Faculty of Mathematics and Physics

This publication has a published version with DOI 10.3390/geosciences13010019

Abstract
This study considers the full waveform inversion (FWI) method based on the asymptotic solution of the Helmholtz equation. We provide frequency-dependent ray tracing to obtain the wave field used to compute the FWI gradient and calculate the modeled data. With a comparable quality of the inverse problem solution as applied to the standard finite difference approach, the speed of the calculations in the asymptotic method is an order of magnitude higher. A series of numerical experiments demonstrate the approach's effectiveness in reconstructing the macro velocity structure of complex media for low frequencies.
Keywords
full waveform inversion, asymptotic, frequency-dependent rays, Helmholtz equation,
Permanent link
https://hdl.handle.net/20.500.14178/2276
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WOS:000915640900001
SCOPUS:2-s2.0-85146806624
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Full text of this result is licensed under: Creative Commons Uveďte původ 4.0 International

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