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14C-age tracers in global ocean circulation models
14C-age global ocean circulation models
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2015/8/6
The natural abundance of 14C in total CO2 dissolved in seawater (DIC) is a property applied to evaluate the water age structure and circulation in the ocean and in ocean models. In this study we use t...
Surface Thermal Boundary Condition for Ocean Circulation Models
Surface Thermal Boundary Condition Ocean Circulation Models
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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 ...
Mixed Layers and Fronts in Simple Ocean Circulation Models
Mixed Layers Simple Ocean Circulation Models Fronts
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2009/2/9
A three-dimensional regime with a differentially heated mixed layer on top of an ideal fluid interior is considered in a situation which corresponds to the interior of the well-known wind-driven model...
Parameterizing Eddy-Induced Tracer Transports in Ocean Circulation Models
Eddy-Induced Tracer Transports Ocean Circulation Models
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2008/12/11
It is shown that the effects of mesoscale eddies on tracer transports can be parameterized in a large-scale model by additional advection and diffusion of tracers. Thus, tracers are advected by the ef...
Specification of Eddy Transfer Coefficients in Coarse-Resolution Ocean Circulation Models
Green and Stone Gent and McWilliams Eddy Transfer Coefficients
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2008/11/13
Parametric representations of oceanic geostrophic eddy transfer of heat and salt are studied ranging fromhorizontal diffusion to the more physically based approaches of Green and Stone (GS) and Gent a...
On Haney-Type Surface Thermal Boundary Conditions for Ocean Circulation Models
Thermal Boundary Conditions Ocean Circulation Models Haney-Type
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2008/10/29
Haney-type surface thermal boundary conditions linearly connect net downward surface heat flux Q to air–sea temperature difference (gradient-type condition) ΔT1 or to climate/synoptic sea temperature ...