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-The M.I.T. General Circulation Model (MITgcm) Release 1 contains code for -simulating a wide variety of ocean and atmosphere problems. The model is -compatible with platforms ranging from desktop and commodity -cluster x86 systems to high-end multi-processor supercomputers. Minimum requirements -are a Fortran compiler (the free g77 compiler is sufficient) and a UNIX like -operating system (such as Linux, Solaris, IRIX). -
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-A broad span of example problem -configurations are included in the release. These examples range from planetary scale -circulation simulations of the ocean and atmosphere to high-resolution, small-scale -process studies encompassing non-hydrostatic dynamics. In addition to conventional -prognostic operation, differentiated forms (both tangent-linear and adjoint) -of the MITgcm code can be generated automatically using either the TAMC or TAF -automatic differentiation tools. These derivative forms can be used for dynamical -sensitivity studies and can also be used, together with appropriate optimisation and -control infrastructure, for mathematically rigorous state-estimation and -data-assimilation. A seamless interface to the ECCO group optimisation -environment is available. -
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MITgcm Release 1 Features:

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- - Oceanic and Atmospheric Simulations - -

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- - Automatic Differentiation and Adjoint Sensitivity

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Open Boundaries, Regional and Process Studies

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Packaged Source Repository

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Algorithm and Code Documentation

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- - - + + + + + + MITgcm Sealion Release Home Page + + + +  + + + + +
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Welcome to the web page of release 1 of MITgcm.
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MITgcm  +

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  • +can be used to study both +atmospheric +and +oceanic circulation
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  • +has a +non-hydrostatic +capability
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  • +supports horizontal orthogonal curvilinear coordinates
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  • +has a finite volume treatment of topography
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  • +supports a wide range of physical parameterizations
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  • +has +tangent +linear and adjoint code maintained alongside the forward model
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  • +can run on your pc, workstation or parallel computer using +flexible domain decomposition
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+Here you can: + +
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