Articles | Volume 10, issue 2
https://doi.org/10.5194/gmd-10-765-2017
https://doi.org/10.5194/gmd-10-765-2017
Model description paper
 | 
17 Feb 2017
Model description paper |  | 17 Feb 2017

The Finite-volumE Sea ice–Ocean Model (FESOM2)

Sergey Danilov, Dmitry Sidorenko, Qiang Wang, and Thomas Jung

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Cited articles

Adcroft, A. and Hallberg, R.: On methods for solving the oceanic equations of motion in generalized vertical coordinates, Ocean Model., 11, 224–233, 2006.
Blazek, J.: Computational fluid dynamics: Principles and applications, Elsevier Ltd., 2001.
Campin, J.-M., Adcroft, A., Hill, C., and Marshall, J.: Conservation of properties in a free-surface model, Ocean Model., 6, 221–244, 2004.
Chen, C., Liu, H., and Beardsley, R. C.: An unstructured, finite volume, three-dimensional, primitive equation ocean model: application to coastal ocean and estuaries, J. Atmos. Ocean. Tech., 20, 159–186, 2003.
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Numerical models of global ocean circulation are used to learn about future climate. The ocean circulation is characterized by processes on different spatial scales which are still beyond the reach of present computers. We describe a new model setup that allows one to vary a model's spatial resolution and hence focus the computational power on regional dynamics, reaching a better description of local processes in areas of interest.
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