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Fig 2.14.5a,b.
Calculation of a two-layer model with no-slip conditions on the eastern and western boundaries and slip conditions
on the northern and southern boundaries. The circulation pattern of the upper layer is shown. In the region of the recirculation the
pattern in the lower layer
is similar, i.e. the flow in this region is essentially barotropic. a a calculation with
8tf8M =
2.2. bas in a
but
8tf8M =
4.7. Note the growth of the recirculation gyre
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