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Next: 1.3 Continuous equations in
Up: 1.2 Illustrations of the
Previous: 1.2.8 Ocean biogeochemical cycles
Contents
Figure 1.13 shows MITgcm being used to simulate a
laboratory experiment inquiring into the dynamics of the Antarctic Circumpolar Current (ACC). An
initially homogeneous tank of water (
in diameter) is driven from its
free surface by a rotating heated disk. The combined action of mechanical
and thermal forcing creates a lens of fluid which becomes baroclinically
unstable. The stratification and depth of penetration of the lens is
arrested by its instability in a process analogous to that which sets the
stratification of the ACC.
Figure 1.13:
A numerical simulation (left) of a 1m diameter laboratory
experiment (right) using MITgcm.
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