Hostname: page-component-cd9895bd7-gvvz8 Total loading time: 0 Render date: 2024-12-28T06:23:00.706Z Has data issue: false hasContentIssue false

Slow energy transfer between regions supporting topographic waves

Published online by Cambridge University Press:  21 April 2006

Kalvis M. Jansons
Affiliation:
Department of Mathematics, University College London, Gower Street, London WC1E 6BT, UK
E. R. Johnson
Affiliation:
Department of Mathematics, University College London, Gower Street, London WC1E 6BT, UK

Abstract

In a recent paper (Jansons & Johnson 1988) the authors discuss topographic Rossby waves over a random array of seamounts. It is noted that resonance is possible between a hill and an equal and opposite dale but such resonances are mentioned only briefly due to the small likelihood of correctly matched topography in the ocean. The present paper considers the resonances in detail showing how the normal modes formed by frequency splitting at resonance can be combined to give modes that slowly transfer energy from one region supporting topographic waves, across a region where such weaves are evanescent, to another region supporting waves. In addition to the simplest case of a hill—dale pair for which an exact energy-transferring mode is obtained, transferring modes are given for a three-hill system, for two hills near a coastal boundary, and for two-basin lakes. The analysis is simplified and the results generalized by extensive use of the invariance of the governing equation under conformal mappings. A transferring mode is given for a dale in a random array of seamounts showing energy leaking slowly from the dale to large distances and returning, with the rate of leakage depending on the area fraction of seamounts. It is concluded that although resonances and transferring modes are not likely to be important in random arrays on infinite planes, they are relevant to numerical models, which are necessarily restricted to finite domains, to coastal seamount chains, and to multi-basin lakes.

Type
Research Article
Copyright
© 1988 Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Jansons, K. M. & Johnson, E. R. 1988 Topographic Rossby waves above a random array of seamountains. J. Fluid Mech. 191, 373388.Google Scholar
Johnson, E. R. 1987a Topographic waves in elliptical basins. Geophys. Astrophys. Fluid Dyn. 37, 279296.Google Scholar
Johnson, E. R. 1987b A conformal-mapping technique for topographic-wave problems: semi-infinite channels and elongated basins. J. Fluid Mech. 177, 395405.Google Scholar
LeBlond, P. H. & Mysak, L. A. 1978 Waves in the Ocean, Chap. 5. Elsevier.
Rhines, P. B. 1969 Slow oscillations in an ocean of varying depth. Part 2. Islands and seamounts. J. Fluid Mech. 37, 191205.Google Scholar
Rhines, P. B. & Bretherton, F. 1973 Topographic Rossby waves in a rough-bottomed ocean. J. Fluid Mech. 61, 583607.Google Scholar
Saylor, J. H., Huang, J. C. K. & Reid, R. O. 1980 Vortex modes in southern Lake Michigan. J. Phys. Oceariogr. 10, 18141823.Google Scholar
Schwab, D. J. 1983 Numerical simulation of low-frequency current fluctuations in Lake Michigan. J. Phys. Oceanogr. 13, 22132224.Google Scholar