Hostname: page-component-cd9895bd7-dzt6s Total loading time: 0 Render date: 2024-12-19T23:51:06.608Z Has data issue: false hasContentIssue false
  • English
  • Français

Laboratory models of sea straits

Published online by Cambridge University Press:  12 April 2006

David A. Anati ,
Gad Assaf  and
Rory O. R. Y. Thompson
David A. Anati
Affiliation:
The Weizmann Institute of Science, Rehovot, Israel
Gad Assaf
Affiliation:
The Weizmann Institute of Science, Rehovot, Israel
Rory O. R. Y. Thompson
Affiliation:
The Weizmann Institute of Science, Rehovot, Israel Present address: CSIRO, Division of Atmospheric Physics, Mordialloc, Victoria, Australia.
Get access Rights & Permissions [Opens in a new window]

Abstract

Two basins maintained at different densities are connected by a relatively shallow strait. If the strait is short, the flow is such that the Froude number is unity. The thickness of the intermediate layer, between the outflow and the inflow, is controlled by the requirement that the Richardson number be critical; this thickness is always about one-fifth of the total depth, both in these experiments and in the Strait of Gibraltar. If the strait is long, the Froude number is less than unity in the interior but increases to unity at each end. A strait may be considered short when its length is less than a few hundred times the sill depth.

Type
Research Article
Information
Journal of Fluid Mechanics , Volume 81 , Issue 2 , 24 June 1977 , pp. 341 - 351
Copyright
© 1977 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

Assaf, G. & Hecht, A. 1974 Sea straits: a dynamical model. Deep-Sea Res. 21, 947–958.Google Scholar
Businger, J. A., Wyngaard, J. C., Izumi, Y. & Bradley, E. F. 1971 Flux profile relationships in the atmospheric surface layer. J. Atmos. Sci. 28, 181–189.Google Scholar
Defant, A. 1961 Physical Oceanography, vol. 1. Pergamon.
Mellor, G. L. 1973 Analytic prediction of the properties of stratified planetary surface layers. J. Atmos. Sci. 30, 1061–1069.Google Scholar
Stommel, H. & Farmer, G. H. 1953 Control of salinity in an estuary by a transition. J. Mar. Res. 12, 13–20.Google Scholar
Webb, E. K. 1970 Profile relationships: the log-linear range and extension to strong stability. Quart. J. Roy. Met. Soc. 96, 67–90.Google Scholar