Research Article
Jul 1969

Unsteady Circulation in Shallow, Homogeneous Lakes

Publication: Journal of the Hydraulics Division
Volume 95, Issue 4

Abstract

A method is presented for calculating the three-dimensional, unsteady, wind-driven circulation in a shallow, homogeneous lake on a rotating earth. The equations of motion are linearized, boundary friction is assumed to act only on the bottom; and a constant eddy viscosity is assumed. These approximations assume a shallow lake where a characteristic horizontal dimension is large compared to the maximum depth and where the depth is of the order of magnitude of the Ekman depth of frictional influence or less. The solution can be applied to a lake of arbitrary plan form and bottom topography.

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Published In

Journal of the Hydraulics Division
Volume 95Issue 4July 1969
Pages: 1273 - 1288

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Published in print: Jul 1969
Published online: Feb 3, 2021

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James A. Liggett, M.ASCE
Assoc. Prof. of Civ. Engrg., Cornell Univ., Ithaca, New York

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