Research Article
Aug 1980

Dense Bottom Currents in Rotating Ocean

Publication: Journal of the Hydraulics Division
Volume 106, Issue 8

Abstract

The dynamic equations for a steady dense bottom current on a gently sloping plane in a rotating ocean are outlined. The entrainment and the friction at the wall and the interface respectively are parameterized by making use of the findings for nonrotating dense bottom currents which are summarized. By introducing an appropriate nondimensional length scale, the equations have been solved to yield the discharge, velocity, density, depth, width, densimetric Froude number, etc. along the predicted curved path line of the current. The usefulness of the model is demonstrated by applying it to the Denmark Strait Overflow.

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Journal of the Hydraulics Division
Volume 106Issue 8August 1980
Pages: 1291 - 1308

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Published in print: Aug 1980
Published online: Feb 3, 2021

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Flemming Bo Pedersen
Research Engr., Inst. of Hydrodynamics and Hydr. Engrg., Tech. Univ. of Denmark, Lyngby, Denmark

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