Hostname: page-component-78c5997874-94fs2 Total loading time: 0 Render date: 2024-11-03T04:20:16.115Z Has data issue: false hasContentIssue false
  • English
  • Français

Propagation of internal gravity waves in fluids with shear flow and rotation

Published online by Cambridge University Press:  28 March 2006

Walter L. Jones
Walter L. Jones
Affiliation:
National Center for Atmospheric Research, Boulder, Colorado
Get access Rights & Permissions [Opens in a new window]

Abstract

In a rotating system, the vertical transport of angular momentum by internal gravity waves is independent of height, except at critical levels where the Doppler-shifted wave frequency is equal to plus or minus the Coriolis frequency. If slow rotation is ignored in studying the propagation of internal gravity waves through shear flows, the resulting solutions are in error only at levels where the Doppler-shifted and Coriolis frequencies are comparable.

Type
Research Article
Information
Journal of Fluid Mechanics , Volume 30 , Issue 3 , 29 November 1967 , pp. 439 - 448
Copyright
© 1967 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

Booker, J. R. & Bretherton, F. P. 1967 J. Fluid Mech. 27, 513.
Eady, E. T. 1949 Tellus, 1, 33.
Eliassen, A. & Palm, E. 1961 Geof. Publ. XXII, no. 3, 1.
Hamming, R. W. 1959 J. Ass. Comp. Mach. 6, 37.