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The potential enstrophy conserving form of the linear Coriolis terms
are written:
Here, the Coriolis parameter is defined at vorticity (corner)
points.
The potential enstrophy conserving form of the non-linear Coriolis
terms are written:
The Coriolis terms can also be evaluated together and expressed in
terms of absolute vorticity . The potential enstrophy
conserving form using the absolute vorticity is written:
The
distinction between using absolute vorticity or relative vorticity is
useful when constructing higher order advection schemes; monotone
advection of relative vorticity behaves differently to monotone
advection of absolute vorticity. Currently the choice of
relative/absolute vorticity, centered/upwind/high order advection is
available only through commented subroutine calls.
Next: 2.14.4 Shear terms
Up: 2.14 Vector invariant momentum
Previous: 2.14.2 Kinetic energy
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