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- W2040751808 abstract "A two-dimensional lake breeze model covering both sides of the lake and allowing for simultaneous imposition of synoptic pressure gradients has been developed. The model uses Estoque's techniques for the sea breeze and is essentially the extension of Moroz's lake breeze model with modifications in the treatment of the continuity equation, eddy diffusivity, boundary conditions and the numerical scheme. The model is applied to the cross-section of Lake Ontario at Toronto with the prevailing wind from the northwest and perpendicular to the shore. The ground temperature record at Guelph, which is sufficiently far from the lake to be free from lake breeze effect, is used to compute the temperature input to the model. The contours of wind velocities and potential temperature at 1, 9 and 17 h of the model time and the variation of lake frontal distance from the shoreline are presented. The result shows that only one circulation tube with axis parallel to the shoreline is developed over the north-western half of the lake extending a horizontal dimension of 8 km inland and 12 km offshore from the shoreline and a depth of 700 m at midday. The maximum onshore flow velocity in the tube is 5 m s−1. This maximum occurs 4 km inland from the shoreline and 300 m above the ground." @default.
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- W2040751808 date "1975-06-01" @default.
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- W2040751808 title "Mathematical modelling of lake breeze" @default.
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- W2040751808 doi "https://doi.org/10.1016/0004-6981(75)90002-5" @default.
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