... buoyancy terms ( any term containing Fo ) and assuming that dB / ds > dH / ds ' nb h = ( B / H ) ( dQ / ds ) ĥ / ( dQ / ds ) , where ( dQ / ds ) and ( dQ / ds ) , are the horizontal and vertical entrainment rates . This yields 2Q ( d ) ...
Workbook of Thermal Plume Prediction: Submerged discharge. v. 2 Surface discharge
... buoyancy forces lift it upward as shown in the plot . The plume continues to rise until it loses buoyancy or reaches the water surface . Meanwhile , the plume centerline temperature continues to decay as shown in Fig . 5 by the decay ...
Surface Thermal Plumes: Evaluation of Mathematical Models for the Near and Complete Field
... IAGLR , pp . 654-669 ( 1971 ) . 9. T. J. Simons , Development of Numerical Models of Lake Ontario : Part 2 , Proc . 15th Conf . Great Lakes Research , IAGLR , pp . 655-672 ( 1972 ) . 10. D. F. Paskausky , Winter Circulation in Lake ...
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