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  • Waves
  • Elsevier  (3)
  • Massachusetts Institute of Technology and Woods Hole Oceanographic Institution  (2)
  • Universität Karlsruhe  (2)
  • Annual Reviews
  • 2005-2009  (3)
  • 1990-1994  (2)
  • 1980-1984  (2)
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  • 1
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    Massachusetts Institute of Technology and Woods Hole Oceanographic Institution
    Publikationsdatum: 2022-05-25
    Beschreibung: Submitted to the Joint Program in Physical Oceanography in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution September 2006
    Beschreibung: Ocean surface infragravity waves (periods from 20 to 200 s) observed along the southern California coast are shown to be sensitive to the bottom topography of the shelf region, where propagation is linear, and of the nearshore region, where nonlinearity is important. Infragravity waves exchange energy with swell and wind waves (periods from 5 to 20 s) via conservative nonlinear interactions that approach resonance with decreasing water depth. Consistent with previous results, it is shown here that as waves shoal into water less than a few meters deep, energy is transfered from swell to infragravity waves. In addition, it is shown here that the apparent dissipation of infragravity energy observed in the surfzone is the result of nonlinear energy transfers from infragravity waves back to swell and wind waves. The energy transfers are sensitive to the shallow water bottom topography. On nonplanar beach profiles the transfers, and thus the amount of infragravity energy available for reflection from the shoreline, change with the tide, resulting in the tidal modulation of infragravity energy observed in bottom-pressure records on the continental shelf. The observed wave propagation over the shelf topography is dominated by refraction, and the observed partial reflection from, and transmission across, a steep-walled submarine canyon is consistent with long-wave theory. A generalized regional model incorporating these results predicts the observed infragravity wave amplitudes over variable bottom topography.
    Beschreibung: Support from the Office of Naval Research (Coastal Geosciences Program, N00014-02-10145), the National Science Foundation (Physical Oceanography, OCE-0115850),
    Schlagwort(e): Waves ; Ocean bottom
    Repository-Name: Woods Hole Open Access Server
    Materialart: Thesis
    Format: 3634207 bytes
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
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    Massachusetts Institute of Technology and Woods Hole Oceanographic Institution
    Publikationsdatum: 2022-05-26
    Beschreibung: Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution September, 1970
    Beschreibung: A series of laboratory experiments were conducted in a glass wave tank to investigate the propagation of internal gravity waves up a sloping bottom in a fluid with constant Brunt-Vaisala frequency. Measurements of the wave motion in the fluid interior were primarily taken with electrical conductivity probes; measurements in the boundary layer were made with dye streaks and neutrally buoyant particles. The results indicate that, outside of the breaking zone, the amplitude and horizontal wave number of the high-frequency waves increase lineariy with decreasing depth; this is shown to agree with existing linear, inviscid solutions. A zone of breaking or runup is induced by these high-frequency waves well upslope. Shadowgraph observations show that, if the wave characteristics are coincident, or nearly so, with the bottom slope, the upslope propagation of the low-frequency waves causes a line of regularly spaced vortices to form along the slope. Subsequent mixing in the vortex cells creates thin horizontal laminae that are more homogeneous than the adjacent layers. These laminae slowly penetrate the fluid interior, creating a step-like vertical density structure. Available linear theoretical solutions for the velocity in the viscous boundary layer, determined to be valid for certain experimental conditions, are used to develop a criterion for incipient motion of bottom sediment induced by shoaling internal waves. The maximum sediment sizes that can be placed into motion, according to this criterion, are larger than certain mean sediment sizes on the continental margin off New England. This suggests that internal waves might induce initial sediment movement. Speculation about the geological effects of breaking and vortex instabilities is also given. These processes, not definitely measured in the field as yet, might also be conducive to sediment movement.
    Beschreibung: This work was supported by the Office of Naval Research.
    Schlagwort(e): Sediment transport ; Waves
    Repository-Name: Woods Hole Open Access Server
    Materialart: Thesis
    Format: 9729705 bytes
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
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    Elsevier
    In:  Amsterdam, 253 pp., Elsevier, vol. 10, no. 1, pp. 1-40, (ISBN: 3-540-23712-7)
    Publikationsdatum: 1983
    Schlagwort(e): Textbook of geophysics ; Acoustics ; Seismics (controlled source seismology) ; Waves ; Wave propagation
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
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    Universität Karlsruhe
    In:  Princeton, Universität Karlsruhe, vol. 7, no. 1, pp. 443-487, (ISBN 0-89871-560-1)
    Publikationsdatum: 1993
    Schlagwort(e): Borehole geophys. ; Waves ; Anisotropy ; Muller
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
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    Universität Karlsruhe
    In:  Professional Paper, Spannung und Spannungsumwandlung in der Lithosphäre, Berichtsband für die Jahre 1990 - 1992, Teil B, Jülich, Universität Karlsruhe, vol. 4, no. 16, pp. 959-983, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publikationsdatum: 1993
    Schlagwort(e): Moment tensor ; Waves ; Earthquake ; Inversion
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
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    Elsevier
    In:  Amsterdam, Elsevier
    Publikationsdatum: 1980
    Schlagwort(e): Seismology ; Seismics (controlled source seismology) ; Wave propagation ; Waves ; Textbook of geophysics
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
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    Elsevier
    In:  Amsterdam, 652 pp., Elsevier, vol. 39, no. XVI:, pp. 227-235, (0-444-51955-6)
    Publikationsdatum: 2005
    Schlagwort(e): Seismics (controlled source seismology) ; Applied geophysics ; Wave propagation ; plane ; spherical ; and ; cylindrical ; Waves ; in ; isotropic ; and ; transversely ; isotropic ; solids, ; liquid-solid ; models, ; and ; media ; with ; cylindrical ; inclusions ; (boreholes) ; Textbook of geophysics
    Standort Signatur Erwartet Verfügbarkeit
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