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The MITgcm (MIT General Circulation - Model) is a numerical model for - studying the ocean and atmosphere. It is capable of simulating these - fluids at a wide range of scales and can resolve many different - processes. It has a non-hydrostatic capability (Marshall et al., JGR 1997a - & b) and uses the finite volume method to accurately represent the - bottom boundary position (Adcroft et al., MWR 1998).

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The MITgcm (MIT General Circulation + Model) is a numerical model designed for study of the + atmosphere, ocean, and climate. Its non-hydrostatic formulation + enables it to simulate fluid phenomena over a wide range of + scales; its adjoint capability enables it to be applied to + parameter and state estimation problems. By employing fluid + isomorphisms, one hydrodynamical kernel can be used to simulate + flow in both the atmosphere and ocean.

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You are welcome to + download and use MITgcm.

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Papers charting the development of MITgcm can be found here. +

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MITgcm
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News
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January 22, 2004 :

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+ A spectacular movie by Chris Henze of NASA AMES captures the eddy permitting + expanded cube sphere simulation being carried out by Dimitris Menemenlis and others + at JPL with help from core MITgcm team members and staff from NASA AMES. The animation + shows the speed of ocean currents at 15m depth from the simulation, it can be + downloaded here (its 47MB but worth waiting for!). + A second animation with different perspectives and rotation can be downloaded + here. + As described here Dimitris Menemenlis + will be presenting aspects of this calculation at AGU in Portland. + A list of some other AGU 2004 presentation abstracts related to MITgcm can be + found here. +
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December 9th 2003 :