- About
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The Global ETD Search service is a free service for researchers
to find electronic theses and dissertations. This service is
provided by the
Networked Digital Library of Theses and Dissertations.
Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
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Showing 11 to 20 of 107 (0.048 seconds)| 11 |
Vertical resolution effects in a steady long wave modelToth, Garry, 1951- January 1978 (has links)
No description available.
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| 12 |
A barotropic stability study of free and forced planetary waves /Fyfe, John January 1987 (has links)
No description available.
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| 13 |
Numerical study of the nonlinear Rossby wave critical level development in a barotropic zonal flowBéland, Michel January 1977 (has links)
No description available.
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| 14 |
MF radar observations of tides and planetary wavesKovalam, Sujata. January 2000 (has links) (PDF)
Copies of previously published articles inserted. Bibliography: p. 185-200. Data obtained from six radar stations covering a wide latitude range has been used to determine the global distribution of planetary waves and tides. In the process a number of data analyses techniques were considered for their characterisation.
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| 15 |
Modeling of standing long waves with non-linear effectsSpagnol, John Carlo. January 1975 (has links)
No description available.
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| 16 |
Forced Rossby waves in the presence of a nonlinear critical layerRitchie, C. Harold (Charles Harold) January 1982 (has links)
The behavior of Rossby waves on a shear flow in the presence of a nonlinear critical layer is studied, with particular emphasis on the role played by the critical layer in a Rossby wave resonance mechanism. Previous steady analyses are extended to the resonant case and it is found that the forced wave dominates the solution, provided the flow configuration is not resonant for the higher harmonics induced by the critical layer. Numerical simulations for the forced initial value problem show that the solution evolves towards the analysed steady state when conditions are resonant for the forced wave, and demonstrate some of the complications that arise when they are resonant for higher harmonics.
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| 17 |
Planetary waves in the upper atmosphereSalby, Murry Lewis 05 1900 (has links)
No description available.
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| 18 |
Topographically forced waves in a time-dependent flowRivest, Chantal. January 1985 (has links)
No description available.
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| 19 |
A study of forced solitary Rossby waves /Brasnett, Bruce. January 1982 (has links)
No description available.
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| 20 |
Reflection of nonlinear baroclinic Rossby waves at a non- zonal boundary and the driving of secondary mean flows: y Federico Graef ZiehlGraef Ziehl, Federico January 1990 (has links)
Typescript. / Thesis (Ph. D.)--University of Hawaii at Manoa, 1990. / Includes bibliographical references (leaves 279-283) / Microfiche. / xvi, 283 leaves, bound ill. 29 cm
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