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Next: 3.9.3 Discrete Numerical Configuration
Up: 3.9 Baroclinic Gyre MITgcm
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Contents
3.9.2 Equations solved
For this problem
the implicit free surface, HPE (see section ) form of the
equations described in Marshall et. al [39] are
employed. The flow is three-dimensional with just temperature, , as
an active tracer. The equation of state is linear.
A horizontal Laplacian operator
provides viscous
dissipation and provides a diffusive sub-grid scale closure for the
temperature equation. A wind-stress momentum forcing is added to the momentum
equation for the zonal flow, . Other terms in the model
are explicitly switched off for this experiment configuration (see section
3.9.4 ). This yields an active set of equations
solved in this configuration, written in spherical polar coordinates as
follows
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(3.14) |
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0 |
(3.15) |
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0 |
(3.16) |
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0 |
(3.17) |
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(3.18) |
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(3.19) |
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(3.20) |
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0 |
(3.21) |
where and are the components of the horizontal
flow vector on the sphere (
).
The terms
and
are the components of the vertical
integral term given in equation 1.35 and
explained in more detail in section 2.3.
However, for the problem presented here, the continuity relation (equation
3.16) differs from the general form given
in section 2.3,
equation , because the source terms
are all 0.
The pressure field,
, is separated into a barotropic part
due to variations in sea-surface height, , and a hydrostatic
part due to variations in density,
, integrated
through the water column.
The suffices indicate surface layer and the interior of the domain.
The windstress forcing,
, is applied in the surface layer
by a source term in the zonal momentum equation. In the ocean interior
this term is zero.
In the momentum equations
lateral and vertical boundary conditions for the
and
operators are specified
when the numerical simulation is run - see section
3.9.4. For temperature
the boundary condition is ``zero-flux''
e.g.
.
Next: 3.9.3 Discrete Numerical Configuration
Up: 3.9 Baroclinic Gyre MITgcm
Previous: 3.9.1 Overview
Contents
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