Numerical computation of three-dimensional circulation in Lake Erie - A comparison of a free-surface model and a rigid-lid model
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Engineering topics
Publications and source records attributed to Lick, W..
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The steady-state, wind-driven circulation is calculated in a stratified lake composed of two layers having uniform but unequal densities and eddy diffusivities. The position of the thermocline and the velocities in both layers are calculated from an asymptotic solution of the shallow lake equations when the Ekman number in the epilimnion (upper layer) is of order one but the ratio of hypolimnion (lower layer) to epilimnion eddy diffusivities is much less than one. Large differences in the thermocline shape and the velocities occur between the solution for uniform wind stress and the one for unit order wind stress gradients. For the latter solution the hypolimnion eddy diffusivity magnitude and the bottom topography have a large and important effect.
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The steady state wind-driven circulation was numerically calculated in a rectangular stratified lake. The lake is composed of two layers having uniform but unequal densities and eddy diffusivities. The position in thermocline and the three-dimensional velocities in both layers calculated using shallow lake equations. The results show that, as the eddy diffusivity in the hypolimnion is increased, the thermocline tilt and hypolimnetic velocities increase. The effect of the other variables such as wind stress, density, basin length, and mean thermocline depth are also shown.
Steady state wind driven currents velocity in Lake Erie, using shallow lake level model in numerical calculation
Numerical analysis of steady state, wind driven currents in Lake Erie, using shallow lake model
Lake Erie steady state wind driven currents numerical solutions, using shallow lake model for velocity as function of depth and horizontal position
Waves nonlinear propagation in fluids due to convection, reviewing various solution methods
Two variable expansion method applied to ordinary differential equation and two wave propagation problems, comparing results with matched asymptotic expansions and coordinate stretching methods
Mathematical model for calculating steady-state, wind-driven currents in Lake Erie
Wave interference effects for forced harmonic oscillator transitions between unperturbed states