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Circulation in shallow homogeneous lakes
Steady state, wind driven circulation of shallow, homogeneous lake on rotating earth is studied by means of solution of equations of fluid motion; equations are linearized, dissipation is assumed to result only from bottom friction and constant eddy viscosity is employed; solution gives three dimensional circulation patterns for lake of arbitrary plan form and bottom topography; effect of bottom topography is shown in sample calculations. (26329)
Circulation in shallow homogeneous lakes
Steady state, wind driven circulation of shallow, homogeneous lake on rotating earth is studied by means of solution of equations of fluid motion; equations are linearized, dissipation is assumed to result only from bottom friction and constant eddy viscosity is employed; solution gives three dimensional circulation patterns for lake of arbitrary plan form and bottom topography; effect of bottom topography is shown in sample calculations. (26329)
Circulation in shallow homogeneous lakes
ASCE J Hydraul Div
Liggett, J.A. (author) / Hadjitheodorou, C. (author)
1969
12 pages
Article (Journal)
English
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