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Nonlinear Processes in Geophysics An interactive open-access journal of the European Geosciences Union
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Volume 3, issue 2
Nonlin. Processes Geophys., 3, 110–114, 1996
https://doi.org/10.5194/npg-3-110-1996
© Author(s) 1996. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Nonlin. Processes Geophys., 3, 110–114, 1996
https://doi.org/10.5194/npg-3-110-1996
© Author(s) 1996. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  30 Jun 1996

30 Jun 1996

A centre manifold approach to solitary waves in a sheared, stably stratified fluid layer

W. B. Zimmerman1 and M. G. Velarde2 W. B. Zimmerman and M. G. Velarde
  • 1Department of Chemical Engineering, UMIST, Sackville Street, PO Box 88, Manchester M60 1QD, England
  • 2Instituto Pluridisciplinar, Universidad Complutense, Paseo Juan XXIII, No. 1, Madrid 28040 Spain

Abstract. The centre manifold approach is used to derive an approximate equation for nonlinear waves propagating in a sheared, stably stratified fluid layer. The evolution equation matches limiting forms derived by other methods, including the inviscid, long wave approximation leading to the Korteweg- deVries equation. The model given here allows large modulations of the height of the waveguide. This permits the crude modelling of shear layer instabilities at the upper material surface of the waveguide which excite solitary internal waves in the waveguide. An energy argument is used to support the existence of these waves.

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