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Normal mode decomposition of small-scale oceanic motions
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|Title:||Normal mode decomposition of small-scale oceanic motions|
|Keywords:||Internal waves -- Mathematical models|
Gravity waves -- Mathematical models
Vortex-motion -- Mathematical models
|Abstract:||Small-scale oceanic motions are expected to contain both gravity waves and vortical motion. The vortical motion carries the perturbation potential vorticity of the system. Using eigenvectors of the linear equations of motion, the gravity mode and the vortical mode are defined. The vortical mode carries the linear perturbation potential vorticity and is horizontally nondivergent, whereas the gravity mode does not carry the linear perturbation potential vorticity. In an unforced, inviscid, linearized system, the gravity mode reduces to free linear gravity waves and the vortical mode to a steady geostrophic flow. An attempt to separate oceanic measurements into the gravity and vortical modes can be conveniently made using fields of horizontal divergence HD, vortex stretching VS, and relative vorticity RV. Spectra of HD, VS, and RV are estimated using measurements of horizontal velocity and temperature from IWEX. Frequency spectral estimates of area-averaged horizontal divergence HD and relative vorticity RV represent the result of both attenuation and contamination horizontal wavenumber array response functions. The attenuation array response function describes the unresolvable nature of small-scale fluctuations of HD and RV, and the contamination array response function describes the contamination between HD and RV. These two potential problems inhibit the estimation of fluctuations of HD and RV separately. Observed frequency spectra of HD are well represented by the GM-76 model (Cairns and Williams, 1976), whereas significant disagreements are found between spectral estimates of RV and the GM model at small horizontal scales. Frequency spectra of HD and RV of the GM model are very sensitive to the high wavenumber cutoff. Since the cutoff is not well determined to date, observed discrepancies do not conclusively imply the failure of linear internal wave theory. strikingly well with the GM-76 spectrum model. This agreement suggests that fluctuations at vertical scales greater than 68 m (the smallest resolvable scale) are mainly the gravity mode component. Vertical wavenumber spectra of VS and IR also agree with previous observations by Gregg (1977) and by Gargett et al. (1981). A general scheme to separate the relative vorticity and horizontal kinetic energy spectra into gravity and vortical modes is proposed. This requires horizontal wavenumber-frequency spectra of uncontaminated HD and RV which can be obtained by measuring horizontal velocity components along a closed contour, or with a horizontal space lag smaller than the scale of HD and RV.|
|Description:||Thesis (Ph. D.)--University of Hawaii at Manoa, 1990.|
Includes bibliographical references (leaves 125-128)
xii, 128 leaves, bound ill. 29 cm
|Rights:||All UHM dissertations and 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 from the copyright owner.|
|Appears in Collections:||Ph.D. - Oceanography|
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