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Surface Thermal Boundary Condition for Ocean Circulation Models
Surface Thermal Boundary Condition Ocean Circulation Models
2009/3/9
By employing a heat budget analysis appropriate to zonally and time averaged conditions within the atmosphere, it is shown that the net downward heat flux Q at the ocean's surface can be expressed as ...
Application of a “Radiation-Type” Boundary Condition to the Wave, Porous Bed Problem
Radiation-Type Porous Bed Problem Boundary Condition
2009/3/7
The problem of a small-amplitude wave propagating over a flat porous bed is reanalyzed subject to the bottom boundary condition where u represents the horizontal velocity in the fluid,s represents the...
Real Freshwater Flux as a Natural Boundary Condition for the Salinity Balance and Thermohaline Circulation Forced by Evaporation and Precipitation
Freshwater flux Salinity Balance Natural Boundary Thermohaline Circulation
2008/12/19
Freshwater flux used as a natural boundary condition for the salinity balance is applied to a primitive equation model of the oceanic general circulation. Instead of the relaxation condition or the vi...
On the Mellor–Yamada Turbulence Closure Scheme：The Surface Boundary Condition for q2
Craig and Banner boundary condition Mellor–Yamada boundary condition
2008/12/3
A numerical model that uses a level-2½ turbulence closure scheme is used to compare two boundary conditions for the turbulent energy at the air–sea interface. One boundary condition, the most c...
On the Mellor–Yamada Turbulence Closure Scheme：The Surface Boundary Condition for q2
Mellor–Yamada Turbulence Closure Scheme Surface Boundary Condition
2008/11/26
A numerical model that uses a level-2½ turbulence closure scheme is used to compare two boundary conditions for the turbulent energy at the air–sea interface. One boundary condition, the most c...
Boundary Condition of the Sverdrup Solution from Flow Energetics
Sverdrup Solution Flow Energetics Boundary
2008/11/12
The energetics of the wind-driven, quasigeostrophic circulation is used to rule out the vanishing of the Sverdrup solution in the western boundary of the ocean, apart from the total solution near the ...