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A comparison of numerical and analytical methods for the reduced wave equation with multiple spatial scales

dc.contributor.authorBoyd, John P.en_US
dc.date.accessioned2006-04-10T14:40:29Z
dc.date.available2006-04-10T14:40:29Z
dc.date.issued1991-07en_US
dc.identifier.citationBoyd, John P. (1991/07)."A comparison of numerical and analytical methods for the reduced wave equation with multiple spatial scales." Applied Numerical Mathematics 7(6): 453-479. <http://hdl.handle.net/2027.42/29258>en_US
dc.identifier.urihttp://www.sciencedirect.com/science/article/B6TYD-45D9TD0-13/2/87c4f0ab511dfb1365f9a3eebd70f8b3en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/29258
dc.description.abstractWe compare four different techniques for solving the ordinary differential equation uxx +/- u = [finite part integral]([var epsilon]x) on the unbounded interval, x [set membership, variant] [-[infinity], [infinity]], when [finite part integral]([var epsilon]x) decays rapidly as |x| --&gt; [infinity]. This problem, although very simple, is representative of problems that arise in such diverse fields as numerical weather prediction, plasma physics, and weakly non-local solitary waves. When [var epsilon] We find that the perturbation series is asymptotic but almost always divergent. The effectiveness of the other methods depends on the sign of the coefficient in the differential equation. When the sign is negative, u(x) decays rapidly as |x| --&gt; [infinity]. Pade approximants converge and the rational Chebyshev pseudospectral method is very accurate. One might suppose that the numerical method would be ineffective for small [var epsilon] because of the difficulty of simultaneously resolving two very disparate length scales. However, because that part of u(x) which varies on the "fast" O(1) scale is exponentially small in 1/[var epsilon], as few as twenty basis functions give six decimal place accuracy for a smooth [finite part integral](x) for all [var epsilon].When the sign of the differential equation is negative, u(x) is oscillatory as |x| --&gt; [infinity] (with an amplitude [alpha] which is proportional to exp(-q/[var epsilon]) for some constant q). Pade approximants and the Chebyshev method do not converge, but instead have an accuracy which is limited to O([alpha]). When a special "radiation function" is added to the spectral basis, however, it is possible to obtain arbitrarily high accuracy. The numerically computed coefficient of the radiation function is an accurate approximation to the amplitude of the asymptotic radiation, [alpha]([var epsilon]).en_US
dc.format.extent2075266 bytes
dc.format.extent3118 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypetext/plain
dc.language.isoen_US
dc.publisherElsevieren_US
dc.titleA comparison of numerical and analytical methods for the reduced wave equation with multiple spatial scalesen_US
dc.typeArticleen_US
dc.rights.robotsIndexNoFollowen_US
dc.subject.hlbsecondlevelMathematicsen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumDepartment of Atmospheric, Oceanic & Space Physics and Laboratory for Scientific Computation, University of Michigan, 2455 Hayward Avenue, Ann Arbor, MI 48109, USAen_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/29258/1/0000315.pdfen_US
dc.identifier.doihttp://dx.doi.org/10.1016/0168-9274(91)90038-2en_US
dc.identifier.sourceApplied Numerical Mathematicsen_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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