WHY   ISOPYCNIC   MODELING?
 
 
Fluid dynamics equations typically are of the form                   
 
ut  = aux + buy + cuz + euxx + fuyy + guzz

|<-- 
 

Transport
terms 
(Primary)

 -->|
 

|<--- 
 

Diffusion
terms
(Secondary)

 --->|
 

  
Transport
terms:

In quasi-steady flows, these tend to cancel. This happens both in reality and in the model. However, the balance of vertical and horizontal terms will differ between model and reality due to truncation errors. So will the circulation. 

Diffusion
terms:

The main error source here is numerically induced diapycnal mixing. It can be suppressed by aligning the axes of the mixing tensor with (locally referenced) isopycnals. Rotating the tensor axes, unfortunately, does not reduce transport errors.

 

 By suppressing the term  cuz  and evaluating (aux +  buy ) along isopycnals, 
 isopycnic coordinate models ... 
  • avoid inconsistencies between vertical and horizontal transport terms that cause (among other things) false diapycnal mixing;
  • hide truncation errors associated with horizontal transport behind the "smoke screen" of isopycnal mixing.
     
 
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   Last revised: 8 April 1999