source: NEMO/branches/2019/fix_vvl_ticket1791/doc/latex/NEMO/main/foreword.tex @ 11712

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\chapter*{Foreword}

The ocean engine of NEMO (Nucleus for European Modelling of the Ocean) is a primitive equation model adapted to
regional and global ocean circulation problems.
It is intended to be a flexible tool for studying the ocean and its interactions with the others components of
the earth climate system over a wide range of space and time scales.

Prognostic variables are the three-dimensional velocity field, a non-linear sea surface height,
the \textit{Conservative} Temperature and the \textit{Absolute} Salinity.
In the horizontal direction, the model uses a curvilinear orthogonal grid and in the vertical direction,
a full or partial step $z$-coordinate, or $s$-coordinate, or a mixture of the two.
The distribution of variables is a three-dimensional Arakawa C-type grid.
Various physical choices are available to describe ocean physics, including TKE, and GLS vertical physics.

Within NEMO, the ocean is interfaced with a sea-ice model (SI$^3$)
 %or \href{https://github.com/CICE-Consortium/CICE}{CICE}),
passive tracer and biogeochemical models (TOP-PISCES) and,
via the \href{https://portal.enes.org/oasis}{OASIS} coupler, with several atmospheric general circulation models.
It also support two-way grid embedding via the \href{http://agrif.imag.fr}{AGRIF} software.