 MITgcm has been designed for study of both small and
large-scales in the atmosphere and ocean.
Its non-hydrostatic capability allows it to address
small-scale process, such as
convection
and mixing over topography.
Its use of fluid isomorphisms enables the same hydro dynamical
kernel to be used for study of both
atmospheric
and
oceanic
phenomenon.
Its adjoint capability enable one to study
parameter
sensitivity and
state
estimation.
Read here about applications in:
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