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A note on the slope of a density interface between two stably stratified fluids under wind

Published online by Cambridge University Press:  12 April 2006

Jin Wu
Affiliation:
College of Marine Studies, University of Delaware, Newark

Abstract

Experiments were conducted with two layers of stably stratified fluid in a wind-wave tank. The slope of the density interface was measured and was related to the wind stress, the density difference between the two fluids and the depth of the interface.

Type
Research Article
Copyright
© 1977 Cambridge University Press

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References

Baines, W. D. & Knapp, D. J. 1965 Wind driven water currents. J. Hyd. Div. A.S.C.E. 91, 205221.Google Scholar
Hellström, B. 1941 Wind effect on lakes and rivers. Ingen Vetensk Akad. Handl. 158, 1188.Google Scholar
Keulegan, G. H. 1958 Twelfth progress report on model laws for density currents — the motion of saline fronts in still water. Nat. Bur. Stand. Rep. no. 5831.Google Scholar
Keulegan, G. H. 1966 The mechanics of an arrested saline wedge. In Estuary and Coastline Hydrodynamics (ed. A. T. Ippen), pp. 546574. McGraw-Hill.
Turner, J. S. 1973 Buoyancy Effects in Fluids. Cambridge University Press.
Wu, J. 1969 Laboratory results of salt water intrusion. J. Hyd. Div. A.S.C.E. 95, 22092213.Google Scholar
Wu, J. 1973 Wind-induced turbulent entrainment across a stable density interface. J. Fluid Mech. 61, 275288.Google Scholar
Wu, J. 1975 Wind-induced drift currents. J. Fluid Mech. 68, 4970.Google Scholar