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dc.contributor.advisorDick K.P. Yue and Yuming Liu.en_US
dc.contributor.authorAlam, Mohammad-Rezaen_US
dc.contributor.otherMassachusetts Institute of Technology. Dept. of Mechanical Engineering.en_US
dc.date.accessioned2009-08-26T16:33:49Z
dc.date.available2009-08-26T16:33:49Z
dc.date.copyright2008en_US
dc.date.issued2008en_US
dc.identifier.urihttp://hdl.handle.net/1721.1/46487
dc.descriptionThesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Mechanical Engineering, 2008.en_US
dc.descriptionIncludes bibliographical references (leaves 273-282).en_US
dc.description.abstractIn the first part of this thesis, the mechanisms of nonlinear resonant interaction of surface-interfacial waves with a rippled bottom in a two-layer density stratified fluid in two dimensions is investigated via perturbation analyses and direct simulation. Three classes of Bragg resonances are found to exist if the nonlinear interactions up to third order in the wave/ripple steepness are considered. At second order, class I Bragg resonance occurs involving two surface and/or internal waves and one bottom ripple component. At third order, class II and III Bragg resonances occur involving resonant interactions of four wave/ripple components. A powerful high-order spectral (HOS) method for nonlinear gravity wave dynamics in a homogeneous fluid is extended to the case of a two-layer fluid over non-uniform bottom. The method is capable of capturing the nonlinear interactions among large number of surface/interfacial wave mode and bottom ripple components up to an arbitrary high order. As an illustration of the usefulness of the numerical method a somewhat complicated problem involving many wave/bottom components is considered and it is shown that the ensuing multiple (near) resonant interactions result in the generation of multiple new transmitted/reflected waves that fill a broad wavenumber band eventually leading to loss of order and chaotic motion. In the second part of this thesis, Resonance between waves of an oscillating/translating disturbance in two-layer density stratified fluids is studied. Waves in homogeneous fluid are known to be non-resonant at the second order. Many seas and oceans, however, are weakly stratified. Here it is shown that in the presence of stratification triad resonance between ship-generated waves can occur. For the more general problem and as an independent validation, the HOS is extended to consider the effect of the current and an oscillating submerged singularity. Direct simulation results compare well with analytical predictions in the near- and far-fields and offer a powerful tool for practical problems with general time-dependent motions/interactions of one or more bodies.en_US
dc.description.statementofresponsibilityby Mohammad-Reza Alam.en_US
dc.format.extent282 leavesen_US
dc.language.isoengen_US
dc.publisherMassachusetts Institute of Technologyen_US
dc.rightsM.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.en_US
dc.rights.urihttp://dspace.mit.edu/handle/1721.1/7582en_US
dc.subjectMechanical Engineering.en_US
dc.titleInteraction of waves in a two-layer density stratified fluiden_US
dc.typeThesisen_US
dc.description.degreePh.D.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Mechanical Engineering
dc.identifier.oclc399892647en_US


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