2016
DOI: 10.1080/09205071.2015.1129915
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Efficient computation of Sommerfeld integral tails – methods and algorithms

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Cited by 103 publications
(54 citation statements)
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“…In Figures 2 and 3 are plotted far-field patterns for the seawater and gold problems, respectively, computed by rigorous integration of Sommerfeld integrals (Michalski, 1998;Michalski & Mosig, 2016b) (solid line) and by the second-order saddle-point method (MSP2) of the present paper (dashed line), although these two results are visually indistinguishable. The fields are computed at a fixed radial distance of k 0 r =100 for elevation angles between 0 ∘ (the z axis) and 90 ∘ (the surface) and are plotted normalized to the maximum values using decibel (dB) scale, with the sin and cos functions set to unity.…”
Section: Sample Numerical Results and Validationmentioning
confidence: 86%
“…In Figures 2 and 3 are plotted far-field patterns for the seawater and gold problems, respectively, computed by rigorous integration of Sommerfeld integrals (Michalski, 1998;Michalski & Mosig, 2016b) (solid line) and by the second-order saddle-point method (MSP2) of the present paper (dashed line), although these two results are visually indistinguishable. The fields are computed at a fixed radial distance of k 0 r =100 for elevation angles between 0 ∘ (the z axis) and 90 ∘ (the surface) and are plotted normalized to the maximum values using decibel (dB) scale, with the sin and cos functions set to unity.…”
Section: Sample Numerical Results and Validationmentioning
confidence: 86%
“…However, for a finite scatterer the spectral domain is continuous and now the poles and oscillations along the branch cuts are hard to discretize (Dilz and Beurden 2016, 2017). Deformations of the Sommerfeld integration path to a complex-plane path (Ruiter 1981; Newman and Forrai 1987; Hochman and Leviatan 2010; Michalski and Mosig 2016) can help to evade these poles and branch cuts. In Dilz and Beurden (2017) an algorithm for two-dimensional electromagnetic scattering with TE polarization in a multilayered medium is presented, where both contrast-current density and scattered field are represented on a path in the complex plane of the spectral domain.…”
Section: Introductionmentioning
confidence: 99%
“…The classical layer Green functions and associated Sommerfeld integrals automatically enforce the relevant transmission conditions on the unbounded flat surfaces and thus reduce the scattering problems to integral equations on the obstacles and/or defects (cf. [19,24]). The Sommerfeld integrals amount to singular Fourier integrals [8,25] whose evaluation is generally quite challenging.…”
Section: Introductionmentioning
confidence: 99%