Application of k-epsilon turbulence models to enclosed basins: The role of internal seiches
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[1] Vertical overturns, produced by turbulence in density-stratified lakes and oceans, are often quantified by the Thorpe scale, L-T. The correlation between L-T and the Ozmidov (energy-containing) scale can be used to estimate rates of turbulent dissipati ...
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American Society of Limnology and Oceanography2002
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International Institute of Refrigeration IIR-IIF2001