1998
DOI: 10.1007/s001620050105
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Numerical Computations and Integrations of the Wave Resistance Green's Function

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Cited by 3 publications
(8 citation statements)
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“…2 shows the wave resistance coefficient on the ellipsoid versus the Froude number with 2b/f = 0.8. Our results, in good agreement with those of [2] (steady), show that linear methods [16] overestimate the wave resistance in the high Froude number range. For the same calculations with finite water height (h/f = 2) but with the same value of the submersion depth of the ellipsoid, the coefficient is greatly increased.…”
Section: Abridged English Versionsupporting
confidence: 91%
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“…2 shows the wave resistance coefficient on the ellipsoid versus the Froude number with 2b/f = 0.8. Our results, in good agreement with those of [2] (steady), show that linear methods [16] overestimate the wave resistance in the high Froude number range. For the same calculations with finite water height (h/f = 2) but with the same value of the submersion depth of the ellipsoid, the coefficient is greatly increased.…”
Section: Abridged English Versionsupporting
confidence: 91%
“…In [14,15], preliminary calculations on a source-sink set with strength ±µ 0 (submersion f = 1; separated by 0.1f ) have been carried out in order to optimize the calculation parameters. We have checked that the results are in good agreement with those of [16] (steady linear), [17] (unsteady linear) and [12] (unsteady non linear). To avoid generating excessive velocity gradients, it is necessary to use starting functions given by Eq.…”
Section: Abridged English Versionsupporting
confidence: 63%
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“…This allows realization of fast and effective schemes for numerical evaluation of the 'double integral term'. A practical numerical implementation can be found in [42]; further development for the efficacy and accuracy in computation of the near-field term is described in [50].…”
Section: Introductionmentioning
confidence: 99%
“…However, the summation of such series is not a trivial computational task, it leads to poor accuracy when the source and the field points are close to the free-surface, the method is vulnerable to severe numerical problems because of the presence of very large in magnitude alternating terms and the criteria to choose one of the expansions is difficult to determine. Details of numerical algorithms using the expansions, discussion of their applicability and heuristic criteria of choice between the algorithms can be found in [2,3,38,50]. Another approach in [61] to calculation of the wavelike term is also based on the Green's function representation [5] but the work is in terms of integrals as opposed to the use of the series.…”
Section: Introductionmentioning
confidence: 99%