There have been no small angle approximations (i.e., S << 1) made in
computing the representation Km n. Therefore, for modeling the
physical process of diffusion employing the isopycnal diffusive mixing
hypothesis in the z-level frame, Km n given here is the
form of the diffusion tensor to be used. In so doing, the physics of
diapycnal diffusion is isolated in the parameter
.
The
small angle approximation of Cox (1987) is an additional statement
regarding the behavior of the bulk of the ocean (that isopycnals have
only a rather small slope except in convection regions). This
approximation recovers the form quoted in Gent and McWilliams (1990)
As the small angle approximation is commonly used, it is perhaps
interesting to ask the following question: Given the small angle
approximation representation of the diffusion tensor in the z-level
frame, what is the representation of this tensor in the orthonormal
isopycnal frame? This tensor cannot be the diagonal form given in
equation (B.45) since that form transformed into
the full non-small angle representation of equation
(B.50). Using the full transformation back to the
orthonormal isopycnal frame,
,
or in matrix form
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(42.57) | ||
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![]() |
(42.58) |
![]() |
(42.59) |