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MIT General Circulation Model

The MIT General Circulation Model (MITgcm) is a numerical computer code that solves the equations of motion governing the ocean or Earth's atmosphere… 
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Data assimilationFinite volume methodList of ocean circulation models

Papers overview

Semantic Scholar uses AI to extract papers important to this topic.
2018
2018
Estimates of Internal Tide Energetics in the Western Bay of Bengal
In this paper, a study is presented on energetics of internal tides using available high temporal resolution in situ data… 
2017
2017
Stable water isotopes in the MITgcm (checkpoint 64w)
We present the first results of the implementation of stable water isotopes in the ocean general circulation model MITgcm. The… 
2016
2016
On generation and evolution of seaward propagating internal solitary waves in the northwestern South China Sea
2014
2014
Transformation of internal waves at the bottom ledge
Transformation of internal gravity waves on the oceanic shelf is studied theoretically and numerically within the framework of… 
2012
2012
Estimating Pine Island Ice Shelf melt rates from hydrography and an ocean circulation model
The fast flowing ice stream of the Pine Island Glacier (PIG) in West Antarctica feeds the Pine Island Ice Shelf (PIIS). Its flow… 
2011
2011
Adjoint Sensitivity of the Nino-3 Surface Temperature to Wind Forcing
Theevolutionof sea surface temperature (SST) overthe easternequatorialPacific playsa significant rolein the intense tropicalair… 
2011
2011
Internal Waves in Straits (IWISE): Observations of Wave Generation
Abstract : The long term goals are to use observations and analysis of stratified flow past complex topography to understand how… 
2010
2010
Quantifying Last Glacial Maximum ocean circulation by state estimation
The Last Glacial Maximum (LGM, ∼19,00023,000 years before present) cold period is ideally suited for evaluating the response of… 
2009
2009
Constructing an idealized model of the North Atlantic Ocean using slippery sacks
2004
2004
Eastern equatorial Pacific Ocean T‐S variations with El Niño
Temperature‐Salinity (T‐S) relationship variability in the pycnocline of the eastern equatorial Pacific Ocean (NINO3 region, 5°S… 
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