Articles | Volume 10, issue 2
https://doi.org/10.5194/gmd-10-765-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/gmd-10-765-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The Finite-volumE Sea ice–Ocean Model (FESOM2)
Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
A. M. Obukhov Institute of Atmospheric Physics RAS, Moscow, Russia
Dmitry Sidorenko
Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
Qiang Wang
Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
Thomas Jung
Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
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- Sensitivity of deep ocean biases to horizontal resolution in prototype CMIP6 simulations with AWI-CM1.0 T. Rackow et al. 10.5194/gmd-12-2635-2019
- East Asian summer precipitation in AWI‐CM3: Comparison with observations and CMIP6 models J. Shi et al. 10.1002/joc.8075
- Large-scale sea ice–Surface temperature variability linked to Atlantic meridional overturning circulation P. Vaideanu et al. 10.1371/journal.pone.0290437
- On the Damping Time Scale of EVP Sea Ice Dynamics S. Danilov et al. 10.1029/2021MS002561
- Non-linear aspects of the tidal dynamics in the Sylt-Rømø Bight, south-eastern North Sea V. Fofonova et al. 10.5194/os-15-1761-2019
- On the length and intensity of the West African summer monsoon during the last interglacial African humid period X. Shi et al. 10.1016/j.quascirev.2024.108542
- Scalability and some optimization of the Finite-volumE Sea ice–Ocean Model, Version 2.0 (FESOM2) N. Koldunov et al. 10.5194/gmd-12-3991-2019
- Scale Analysis on Unstructured Grids: Kinetic Energy and Dissipation Power Spectra on Triangular Meshes S. Juricke et al. 10.1029/2022MS003280
- Shifts of the Recirculation Pathways in Central Fram Strait Drive Atlantic Intermediate Water Variability on Northeast Greenland Shelf R. McPherson et al. 10.1029/2023JC019915
- Atmospheric blocking slows ocean-driven melting of Greenland’s largest glacier tongue R. McPherson et al. 10.1126/science.ado5008
- A Scalable Semi‐Implicit Barotropic Mode Solver for the MPAS‐Ocean H. Kang et al. 10.1029/2020MS002238
- Discrete variance decay analysis of spurious mixing T. Banerjee et al. 10.1016/j.ocemod.2024.102460
- Evaluation of FESOM2.0 Coupled to ECHAM6.3: Preindustrial and HighResMIP Simulations D. Sidorenko et al. 10.1029/2019MS001696
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Latest update: 15 Nov 2024
Short summary
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.
Numerical models of global ocean circulation are used to learn about future climate. The ocean...