Direct and Large Eddy Simulation of Turbulent Heat Transfer at Very Low Prandtl Number: Application to Lead-bismuth Flows Laurent Bricteux1 , Matthieu Duponcheel 1 , Yann Bartosiewicz1 1 Universit´e catholique de Louva

Source URL: www.djs.si

KATABATIC FLOW WITH CORIOLIS EFFECT AND GRADUALLY VARYING EDDY DIFFUSIVITY IVA KAVČIČ* Department of Geophysics, Faculty of Science, University of Zagreb, Croatia BRANKO GRISOGONO Department of Geophysics, Faculty of S

Source URL: bib.irb.hr

• Heat transfer
• Oceanography
• Convection
• Turbulent Prandtl number
• Partial differential equation
• Boundary layer
• Ekman layer
• Coriolis effect
• WKB approximation
• Physics
• Meteorology
• Atmospheric sciences

QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 133: 101–[removed]Published online in Wiley InterScience (www.interscience.wiley.com) DOI: [removed]qj.19 Including Coriolis effects in th

Source URL: bib.irb.hr

• Coriolis effect
• Force
• Physical phenomena
• Partial differential equation
• Turbulent Prandtl number
• Boundary layer
• Sine
• Differential equation
• Physics
• Heat transfer
• Mechanical engineering

MAY[removed]JACKSON ET AL. 1033

Source URL: www.gfdl.noaa.gov

• Turbulence
• Richardson number
• Turbulence kinetic energy
• Turbulent Prandtl number
• Law of the wall
• Large eddy simulation
• Viscosity
• Plume
• Reynolds number
• Physics
• Fluid dynamics
• Fluid mechanics

Atm S 547 Boundary Layer Meteorology Bretherton

Source URL: www.atmos.washington.edu

• Oceanography
• Heat transfer
• Air dispersion modeling
• Aquatic ecology
• Ekman layer
• Surface layer
• Log wind profile
• Turbulent Prandtl number
• Boundary layer
• Meteorology
• Atmospheric sciences
• Fluid dynamics