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Model Studies of the Wind-Driven Transient Circulation in the Middle Atlantic Bight. Part 1：Adiabatic Boundary Conditions
Wind-Driven Transient Circulation Middle Atlantic Bight Adiabatic Boundary Conditions
2009/2/9
A numerical model of the wind-driven transient ocean circulation in the Middle Atlantic Bight is described. The model incorporates realistic topography and covers the continental shelf between the coa...
Do We Require Adiabatic Dissipation Schemes in Eddy-Resolving Ocean Models?
Adiabatic Dissipation Schemes Eddy-Resolving Ocean Models
2008/10/24
Use of horizontal diffusion of temperature and salinity in numerical ocean models causes spurious diapycnal transfers—the “Veronis effect”—leading to erosion of the thermocline and reduced poleward he...
The Primitive Equations in the Stochastic Theory of Adiabatic Stratified Turbulence
Primitive Equations Stochastic Theory Adiabatic Stratified Turbulence
2008/7/21
The stochastic theory of compressible turbulent fluid transport recently developed by Dukowicz and Smith is applied to the ensemble-mean primitive equations (PEs) for adiabatic stratified flow. The th...
Ultrasonic in situ measurements of density, adiabatic compressibility, and stability frequency
Ultrasonic situ measurements of density adiabatic compressibility stability frequency
2014/5/27
An in situ density profile has been measured with an ultrasonic density probe in the mining lake Merseburg-Ost 1b. From the acquired measurements of sound speed and acoustic impedance, the important p...