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About MITgcm

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.

You are welcome to download and use MITgcm.

Papers charting the development of MITgcm can be found here.

Latest News and Features

Plunging into Early Paleozoic Oceans with MITgcm
Apr 20th, 2017 by Helen Hill

story by Helen Hill

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Late Ordovician-early Silurian continental reconstruction interpolated on the MITgcm cubed sphere grid: AAC: Arctic Alaska-Chukotka, KO: Kolyma-Omolon, A: Avalonia, T: Tarim, NC: North China, SC: South China, An: Annamia. Ocean names are in italics - image courtesy A. Pohl

Late Ordovician-early Silurian continental reconstruction interpolated on the MITgcm cubed sphere grid: AAC: Arctic Alaska-Chukotka, KO: Kolyma-Omolon, A: Avalonia, T: Tarim, NC: North China, SC: South China, An: Annamia. Ocean names are in italics - image courtesy A. Pohl

This month we spotlight new work by Alexandre Pohl and co-authors from France and the UK concerning ocean circulation in deep geological time. Pohl et al used a coupled ocean-atmosphere setup of the MITgcm to investigate the relationships between climate and marine biogeochemistry during the Late Ordovician (445 million years ago).

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Melting Antarctica
Mar 28th, 2017 by Helen Hill

story by Helen Hill

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Shelf ice edge in the Atka Bay, eastern Weddell Sea, off the coast of West Antarctica. Credit: Alfred Wegener Institute/Stefan Hendricks.

Shelf ice edge in the Atka Bay, eastern Weddell Sea, off the coast of West Antarctica. Credit: Alfred Wegener Institute/Stefan Hendricks.

This month we spotlight work led by long time MITgcm associate Alberto C. Naveira Garabato. Using MITgcm, Garabato and his team constructed a suite of idealized modelling experiments to demonstrate that initial ascent of the meltwater outflow from an ice shelf cavity triggers a centrifugal overturning instability that grows by extracting kinetic energy from the lateral shear of the background oceanic flow, promoting vigorous lateral export, rapid dilution by turbulent mixing, and finally settling of meltwater at depth. Read the rest of this entry »

Shelf Slip
Feb 15th, 2017 by Helen Hill

story by Helen Hill

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Scotland_from_space

The Shetland shelf is one side of the Faroe-Shetland Channel: a deep bathymetric channel extending north-eastwards between Scotland and the Faroe Islands - Image: Wikipedia

This month we spotlight work by Arjav Trivedi and Ralf Toumi in the Space and Atmospheric Physics Group, in the Physics Dept. at Imperial College, London, UK, who have been using MITgcm to study the circulation on the Shetland Shelf system. Read the rest of this entry »

2016 Research Roundup
Jan 20th, 2017 by Helen Hill

To round out the year we have again collected a sample of over one hundred research articles published in 2016 that involved MITgcm in some way. Email missing citations or pitch your research to [email protected]. Happy New Year!

1280px-Attheya_longicornis patagonia Fig4_web 13174146_1188986994445256_4121688940383422267_n bas_10002957_roughseasinthesouthernocean
Coccolithophores, among which Emiliania huxleyi (E. huxleyi) is the most abundant and widespread species, are considered to be the most productive calcifying organism on earth. E. huxleyi often forms massive blooms in temperate and sub-polar oceans, and in particular at continental margins and shelf seas - more at mussels-1665863_1920 Southern Ocean temperature (SOSE) - click on the image to see the movie by Uriel Zajaczkovski; http://pordlabs.ucsd.edu/uriel/

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