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| | {{Model identity |
| | |Model type=Modular |
| | }} |
| | {{Model identity2 |
| | |ModelDomain=Climate |
| | |Spatial dimensions=3D |
| | |Spatialscale=Global |
| | |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. |
| | }} |
| | {{Start model keyword table}} |
| | {{End a table}} |
| {{Modeler information | | {{Modeler information |
| |First name=Nicole | | |First name=Nicole |
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| |Postal code=80309 | | |Postal code=80309 |
| |State=Colorado | | |State=Colorado |
| |Country=USA | | |Country=United States |
| |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
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|
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| Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997), Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling, J. Geophysical Res., 102(C3), 5733-5752.
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|
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| 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.
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|
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| 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.
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|
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| Marshall,J.,Jones,H.andC.Hill,(1998), Efficient ocean modeling using non-hydrostatic algorithms, Journal of Marine Systems,18,115-134.
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|
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| 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.
| |
|
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| 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.
| |
|
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| 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 type=Modular
| |
| |Categories=Climate
| |
| |Spatial dimensions=3D
| |
| |Spatialscale=Global
| |
| |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.
| |
| |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 technical information | | {{Model technical information |
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| |Start year development=1997 | | |Start year development=1997 |
| |Does model development still take place?=Yes | | |Does model development still take place?=Yes |
| |Model availability=As executable
| |
| |Source code availability=Through web repository | | |Source code availability=Through web repository |
| |Source web address=http://mitgcm.org/ | | |Source web address=http://mitgcm.org/ |
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| |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 |
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| |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}} |
| | | {{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.
| | {{Documentation model |
| | | |Manual model available=No |
| 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 | |
| | |
| 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}} |
| {{Documentation model | | {{Documentation model |
| |Manual model available=Yes | | |Manual model available=Yes |
| |Model manual=Manual.pdf, | | |Model manual=Manual_MITgcm.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
| |
| | |
| 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.
| |
| }} | | }} |
| {{Additional comments model | | {{Additional comments model |
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| |CCA component=No but possible | | |CCA component=No but possible |
| |IRF interface=No but possible | | |IRF interface=No but possible |
| |CMT component=Not yet | | |CMT component=No but possible |
| }} | | }} |
| | {{Start coupled table}} |
| | {{End a table}} |
| {{End headertab}} | | {{End headertab}} |
| | {{{{PAGENAME}}_autokeywords}} |
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| <!-- PLEASE USE THE "EDIT WITH FORM" BUTTON TO EDIT ABOVE CONTENTS; CONTINUE TO EDIT BELOW THIS LINE --> | | <!-- PLEASE USE THE "EDIT WITH FORM" BUTTON TO EDIT ABOVE CONTENTS; CONTINUE TO EDIT BELOW THIS LINE --> |
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| {{#ifexist:Template:{{#sub:{{PAGENAME}}|0|1}}{{#sub:{{lc:{{PAGENAME}}}}|1}} download stats | ==Download statistics==
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| {{{{#sub:{{PAGENAME}}|0|1}}{{#sub:{{lc:{{PAGENAME}}}}|1}} download stats}} | }}
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| ==Introduction== | | ==Introduction== |
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| == History == | | == History == |
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| == Papers == | | == References == |
| | <br>{{AddReferenceUploadButtons}}<br><br> |
| | {{#ifexist:Template:{{PAGENAME}}-citation-indices|{{{{PAGENAME}}-citation-indices}}|}}<br> |
| | {{Include_featured_references_models_cargo}}<br> |
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| == Issues == | | == Issues == |
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| == Help == | | == Help == |
| | {{#ifexist:Model_help:{{PAGENAME}}|[[Model_help:{{PAGENAME}}]]|}} |
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| == Input Files == | | == Input Files == |
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| == Output Files == | | == Output Files == |
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| == Download ==
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| == Source ==
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