Model:MITgcm: Difference between revisions

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|Country=USA
|Country=USA
|Email address=nicole.lovenduski@colorado.edu
|Email address=nicole.lovenduski@colorado.edu
|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
}}
{{Model identity
{{Model identity
Line 35: Line 19:
|One-line model description=The MITgcm (MIT General Circulation Model) is a numerical model designed for study of the atmosphere, ocean, and climate.
|One-line model description=The MITgcm (MIT General Circulation Model) is a numerical model designed for study of the atmosphere, ocean, and climate.
|Extended model description=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.
|Extended model description=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.
|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
}}
{{Start model keyword table|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
{{Start model keyword table
 
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
 
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
 
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
 
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
}}
{{End a table|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
{{End a table
 
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
 
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
 
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
 
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
}}
{{Model technical information
{{Model technical information
Line 98: Line 36:
|Memory requirements=Memory requirements range from around 10^7 bytes (≈ 10 megabytes) to 10^11 bytes (≈ 100 gigabytes).
|Memory requirements=Memory requirements range from around 10^7 bytes (≈ 10 megabytes) to 10^11 bytes (≈ 100 gigabytes).
|Typical run time=Run time can range from minutes to weeks, depending on length of simulation and size/resolution of domain.
|Typical run time=Run time can range from minutes to weeks, depending on length of simulation and size/resolution of domain.
|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
}}
{{Input - Output description
{{Input - Output description
Line 122: Line 44:
|Post-processing software needed?=No
|Post-processing software needed?=No
|Visualization software needed?=No
|Visualization software needed?=No
|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
}}
{{Process description model
{{Process description model
|Describe processes represented by the model=too many to describe
|Describe processes represented by the model=too many to describe
|Describe key physical parameters and equations=too many to describe
|Describe key physical parameters and equations=too many to describe
|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
}}
{{Model testing|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
{{Model testing
 
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
 
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
 
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
 
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
}}
{{Users groups model|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
{{Users groups model
 
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
 
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
 
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
 
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
}}
{{Documentation model
{{Documentation model
|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
|Manual model available=Yes
|Model manual=Manual.pdf,
|Model website if any=http://mitgcm.org/
|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York  
|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York  


Line 234: Line 75:
http://mitgcm.org/
http://mitgcm.org/
No need to register
No need to register
|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
}}
{{CSDMS staff part
{{CSDMS staff part
Line 256: Line 81:
|IRF interface=No but possible
|IRF interface=No but possible
|CMT component=Not yet
|CMT component=Not yet
|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
{{Start coupled table|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
{{End a table|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
}}
{{End headertab|Provide key papers on model if any=Hill, C. and J. Marshall, (1995), Application of a Parallel Navier-Stokes Model to Ocean Circulation in Parallel Computational Fluid Dynamics, In Proceedings of Parallel Computational Fluid Dynamics: Implementations and Results Using Parallel Computers, 545-552. Elsevier Science B.V.: New York
{{Start coupled table
 
Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
 
Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997), A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers, J. Geophysical Res.,102(C3),5753-5766.
Adcroft,A.J.,Hill,C.N. and J.Marshall,(1997), Representation of topography by shaved cells in a height coordinate ocean model, Mon Wea Rev, vol 125, 2293-2315.
 
Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
 
Adcroft,A.,Hill C.and J.Marshall:(1999), A new treatment of the Coriolis terms in C-grid models at both high and low resolutions, Mon. Wea. Rev. Vol 127, pages 1928-1936.
Hill, C, Adcroft, A., Jamous, D.,and J.Marshall,(1999), A Strategy for Terascale Climate Modeling. In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors in Meteorology, pages 406-425, World Scientific Publishing Co:UK.
Marotzke,J,Giering,R.,Zhang,K.Q.,Stammer,D.,Hill,C.,and T.Lee,(1999),Construction of the adjoint MIT ocean general circulation model and
application to Atlantic heat transport variability, J. Geophysical Res., 104(C12), 29, 529-29,547.
}}
}}
{{End headertab}}
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Revision as of 16:37, 23 June 2011

Name Nicole Lovenduski
Type of contact Project manager
Institute / Organization University of Colorado at Boulder
Postal address 1 Institute of Arctic and Alpine Research
Postal address 2 Campus Box 450
Town / City Boulder
Postal code 80309
State Colorado
Country USA"USA" is not in the list (Afghanistan, Albania, Algeria, Andorra, Angola, Antigua and Barbuda, Argentina, Armenia, Australia, Austria, ...) of allowed values for the "Country" property.
Email address nicole.lovenduski@colorado.edu
Phone
Fax



MITgcm


Metadata

Also known as
Model type Modular
Model part of larger framework
Note on status model
Date note status model
Keywords:
Supported platforms
Unix, Linux, Mac OS
Other platform
Programming language

Fortran90

Other program language
Code optimized Multiple Processors
Multiple processors implemented
Nr of distributed processors
Nr of shared processors
Start year development 1997
Does model development still take place? Yes
If above answer is no, provide end year model development
Code development status
When did you indicate the 'code development status'?
Model availability
Source code availability
(Or provide future intension) 		Through web repository
Source web address http://mitgcm.org/
Source csdms web address
Program license type Other
Program license type other --
Memory requirements Memory requirements range from around 10^7 bytes (≈ 10 megabytes) to 10^11 bytes (≈ 100 gigabytes).
Typical run time Run time can range from minutes to weeks, depending on length of simulation and size/resolution of domain.


Describe input parameters
Input format Binary
Other input format
Describe output parameters
Output format Binary
Other output format NetCDF
Pre-processing software needed? No
Describe pre-processing software
Post-processing software needed? No
Describe post-processing software
Visualization software needed? No
If above answer is yes
Other visualization software


Describe processes represented by the model too many to describe
Describe key physical parameters and equations too many to describe
Describe length scale and resolution constraints
Describe time scale and resolution constraints
Describe any numerical limitations and issues


Describe available calibration data sets
Upload calibration data sets if available:
Describe available test data sets
Upload test data sets if available:
Describe ideal data for testing


Do you have current or future plans for collaborating with other researchers?
Is there a manual available?
Upload manual if available:
Model website if any
Model forum / discussion board
Comments Notice: Code is freely available through the following site:

http://mitgcm.org/ No need to register


This part will be filled out by CSDMS staff

OpenMI compliant No but possible
BMI compliant No but possible
WMT component Not yet"Not yet" is not in the list (Yes, In progress, No but possible, No not possible) of allowed values for the "Code CMT compliant or not" property.
PyMT component
Is this a data component
Can be coupled with:


Model info
Authors
Nicole Lovenduski
Source code
Model citations
Nr. of publications: 121
Total citations: 7898
h-index: 35
m-quotient: 0.74
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Link to this page
Other models by author



Introduction

History

Papers

Issues

Help

Input Files

Output Files

Download

Source
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