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The Global ETD Search service is a free service for researchers
to find electronic theses and dissertations. This service is
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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 1 to 10 of 62 (0.059 seconds)Spelling suggestions: "subject:"atmospheric waves."" "subject:"tmospheric waves.""
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Structures d'ondes forcées sur une sphère en rotationLaprise, René January 1977 (has links)
No description available.
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| 2 |
Simulation temporelle des ondes longues atmosphériquesDesmarais, Jean-Guy January 1977 (has links)
No description available.
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| 3 |
Structures d'ondes forcées sur une sphère en rotationLaprise, René January 1977 (has links)
No description available.
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| 4 |
Simulation temporelle des ondes longues atmosphériquesDesmarais, Jean-Guy January 1977 (has links)
No description available.
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| 5 |
A case study of gravity wave-convective storm interactions, 9 May 1979Stobie, James George 12 1900 (has links)
No description available.
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| 6 |
Meteor radar studies of the mesopause region and nonlinear atmospheric wavesXiao, Jingwei 08 1900 (has links)
No description available.
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Wave disturbances associated with the Red River Valley severe weather outbreak of 10-11 April by Rossella FerrettiFerretti, Rossella 12 1900 (has links)
No description available.
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| 8 |
The effect of weak non-linearity on vertically propagating internal gravity waves in the atmosphere /Ibrahim, Mostafa M. January 1982 (has links)
The linear and weakly non-linear limits of two-dimensional gravity waves in an incompressible, inviscid and stably stratified atmosphere are studied. The linear results indicate the growth of waves propagating upward leading to the breakdown of the linear theory. The three-wave resonant interaction theory indicates an energy cascade from a vertically propagating wave (primary wave) to waves having smaller absolute values of Doppler shifted frequency ((OMEGA)). When the non-dimensional parameter / (DIAGRAM, TABLE OR GRAPHIC OMITTED...PLEASE SEE DAI) / is in the range "1 to about 0.8" (N being the Brunt-Vaisala frequency), the energy of the primary wave is transferred to bands of small amplitude waves. The triads in these bands include a member with the same vertical group velocity as the primary wave while other triads contain a member with larger vertical group velocity. The band widths approach zero as the primary wave amplitude is reduced. The analysis suggests that the three-wave resonant interactions should be replaced by a higher order approximation in this limit.
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| 9 |
Atmospheric gravity waves in constituent distributions / by Dorothy E. Gibson-Wilde.Gibson-Wilde, Dorothy E. January 1996 (has links)
Copies of author's previously published works inserted. / Bibliography: p. 181-195. / xxviii, 195 p. : ill. ; 30 cm. / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Investigated the influence of atmospheric gravity waves on constituents, particularly ozone in the stratosphere and neutral sodium in the mesosphere. / Thesis (Ph.D.)--University of Adelaide, Dept. of Physics and Mathematical Physics, 1997?
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Tropical dynamics near the stratospause : the two-day wave and its relatives /Limpasuvan, Varavut. January 1998 (has links)
Thesis (Ph.D.) University of Washington, 1998. / Vita. Includes bibliographical references (p. [197]-204).
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