2015
DOI: 10.1137/140993648
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A Recursive Algorithm for MultiFrequency Acoustic Inverse Source Problems

Abstract: An iterative/recursive algorithm is studied for recovering unknown sources of acoustic field with multifrequency measurement data. Under additional regularity assumptions on source functions, the first convergence result toward multifrequency inverse source problems is obtained by assuming the background medium is homogeneous and the measurement data is noise-free. Error estimates are also provided when the observation data is contaminated by noise. Numerical examples verify the reliability and efficiency of o… Show more

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Cited by 89 publications
(54 citation statements)
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“…These methods can be classified into two categories: iterative methods and non-iterative methods. While very successful in many cases, iterative methods are usually computationally expensive since they require the solution of a direct problem in every step [2,19]. In contrast, the second group of reconstruction methods, i.e., non-iterative methods, avoids this problem, e.g., [10,11,13,14,17,18].…”
mentioning
confidence: 99%
“…These methods can be classified into two categories: iterative methods and non-iterative methods. While very successful in many cases, iterative methods are usually computationally expensive since they require the solution of a direct problem in every step [2,19]. In contrast, the second group of reconstruction methods, i.e., non-iterative methods, avoids this problem, e.g., [10,11,13,14,17,18].…”
mentioning
confidence: 99%
“…The second one is the numerical error of approximated linearized DtN map Λ in (4.4) where the elliptic equation solvers of large wavenumbers and the numerical differentiation of the Neumann boundary data may induce some additional ill-posedness. The error estimate of Algorithm 1 may be carried out by choosing the length and angle sets following the analysis in [4,5]. We intend to report such results in a separate work.…”
Section: Reconstruction Algorithmmentioning
confidence: 99%
“…Over recent years, intensive attention [6,8,9,16,22,23,24,36,37,38,39] has been focused on the inverse source problem of determining a source F in the Helmholtz equation ∆u + k 2 u = F in Ω, (1.1) from boundary measurements u| Γ and ∂ ν u| Γ , where k > 0 is the wavenumber, Ω ⊂ R N (N = 2, 3) is a bounded Lipschitz domain with boundary Γ and ν denotes the outward unit normal to Γ. A main difficulty of the inverse source problem with a single wavenumber is the non-uniqueness of the source due to the existence of nonradiating sources [3,10,11,15,17], and several numerical methods with multi-frequency measurements [8,9,24,42] have been proposed to overcome it for the source with a arXiv:1801.05584v1 [math.AP] 17 Jan 2018 compact support in the L 2 sense. However, fortunately, with a single wavenumber, the uniqueness can be obtained if a priori information on the source is available [18,23].…”
Section: Introductionmentioning
confidence: 99%