Commit 5918c2f8 authored by Nikolay Koldunov's avatar Nikolay Koldunov
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*.out filter=lfs diff=lfs merge=lfs -text
*.nc filter=lfs diff=lfs merge=lfs -text
*.tar.gz filter=lfs diff=lfs merge=lfs -text
This folder contains one of standard FESOM2 meshes.
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** hr **
source mesh: BOLD_RT_FIXED
contact: D. Sein
topography: RTopo-2.0.1_30sec_global_topo_2016-12-13.nc (https://doi.org/10.5194/essd-8-543-2016) with some modifications.
Reference (please cite when you use this mesh):
Sein, D. V., Danilov, S., Biastoch, A., Durgadoo, J. V., Sidorenko, D., Harig, S., and Wang, Q. (2016), Designing variable ocean model resolution based on the observed ocean variability, J. Adv. Model. Earth Syst., 8, 904– 916, doi:10.1002/2016MS000650.
Sein, D. V., Koldunov, N. V., Danilov, S., Wang, Q., Sidorenko, D., Fast, I., Rackow, T., Cabos, W. and Jung, T., Ocean Modeling on A Mesh with Resolution Following the Local Rossby Radius. Journal of Advances in Modeling Earth Systems, 9, 2601–2614. doi:10.1002/2017MS001099 , 2017
For AWI-CM2 setup also cite: Sidorenko, D., Goessling, H. F., Koldunov, N. V., Scholz, P., Danilov, S., Barbi, D., et al (2019). Evaluation of FESOM2.0 coupled to ECHAM6.3: Pre‐industrial and HighResMIP simulations. Journal of Advances in Modeling Earth Systems, 11. https://doi.org/10.1029/2019MS001696
! NOTE: Topography used for the current mesh is different from the ones used in Sein et al., 2016, 2017. This exact version of the mesh was used in Sidorenko et al., 2019.
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** orca25 **
source mesh: NEMO_RT_FIXED
contact: N. Koldunov
topography: RTopo-2.0.1_30sec_global_topo_2016-12-13.nc (https://doi.org/10.5194/essd-8-543-2016) with some modifications.
Reference (please cite when you use this mesh): Juricke, S., Danilov, S., Koldunov, N. V., Oliver, M., & Sidorenko, D. (2020). Ocean kinetic energy backscatter parametrization on unstructured grids: Impact on global eddy‐permitting simulations. Journal of Advances in Modeling Earth Systems, 12, e2019MS001855. https://doi.org/10.1029/2019MS001855
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** core2 **
source mesh: core2_meanz
topography: A blend of several bottom topography data sets (see Wang et al., 2014).
Reference (please cite when you use this mesh):
Wang, Q., Danilov, S., Sidorenko, D., Timmermann, R., Wekerle, C., Wang, X., Jung, T., and Schröter, J.: The Finite Element Sea Ice-Ocean Model (FESOM) v.1.4: formulation of an ocean general circulation model, Geosci. Model Dev., 7, 663–693, https://doi.org/10.5194/gmd-7-663-2014, 2014.
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** core2_old **
source mesh: mesh_CORE2_finaltopo_mean
topography: A blend of several bottom topography data sets (see Wang et al., 2014).
Reference (please cite when you use this mesh):
Wang, Q., Danilov, S., Sidorenko, D., Timmermann, R., Wekerle, C., Wang, X., Jung, T., and Schröter, J.: The Finite Element Sea Ice-Ocean Model (FESOM) v.1.4: formulation of an ocean general circulation model, Geosci. Model Dev., 7, 663–693, https://doi.org/10.5194/gmd-7-663-2014, 2014.
! NOTE: The only reason to use this mesh is to reproduce AWI-CM2 setup from Sidorenko et al., 2019. In other cases DONT USE IT!
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** farc **
source mesh: farc_sorted
contact: W. Wang
topography: IBCAO and GEBCO (see details in Wang et al., 2018)
Reference (please cite when you use this mesh): Wang, Q., Wekerle, C., Danilov, S., Wang, X., and Jung, T.: A 4.5 km resolution Arctic Ocean simulation with the global multi-resolution model FESOM 1.4, Geosci. Model Dev., 11, 1229–1255, https://doi.org/10.5194/gmd-11-1229-2018, 2018.
! NOTE The nodes in this mesh was sorted, which is different from the version of Wang et al., 2018
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** pi **
source mesh: pi_mesh
contact: T. Rakow
topography:
Reference:
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** mr **
source mesh: mr
contact: D. Sein
Reference:
Sein, D. V., Danilov, S., Biastoch, A., Durgadoo, J. V., Sidorenko, D., Harig, S., and Wang, Q. (2016), Designing variable ocean model resolution based on the observed ocean variability, J. Adv. Model. Earth Syst., 8, 904– 916, doi:10.1002/2016MS000650.
Sein, D. V., Koldunov, N. V., Danilov, S., Wang, Q., Sidorenko, D., Fast, I., Rackow, T., Cabos, W. and Jung, T., Ocean Modeling on A Mesh with Resolution Following the Local Rossby Radius. Journal of Advances in Modeling Earth Systems, 9, 2601–2614. doi:10.1002/2017MS001099 , 2017
For AWI-CM1 setup also cite: Semmler, T., Danilov, S., Gierz, P., Goessling, H. F., Hegewald, J., Hinrichs, C., et al. (2020). Simulations for CMIP6 with the AWI climate model AWI‐CM‐1‐1. Journal of Advances in Modeling Earth Systems, 12, e2019MS002009. https://doi.org/10.1029/2019MS002009
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zaxistype = depth_below_sea
size = 47
levels = 2.5 7.5 15 25 35 45 55 65 75 85 95 107.5 125 147.5 175 210 255 310 375 450 535 630 735 850 975 1110 1255 1415 1600 1810 2035 2275 2525 2775 3025 3275 3525 3775 4025 4275 4525 4775 5025 5275 5525 5825 6125
lbounds = 5 10 20 30 40 50 60 70 80 90 100 115 135 160 190 230 280 340 410 490 580 680 790 910 1040 1180 1330 1500 1700 1920 2150 2400 2650 2900 3150 3400 3650 3900 4150 4400 4650 4900 5150 5400 5650 6000 6250
ubounds = 0 5 10 20 30 40 50 60 70 80 90 100 115 135 160 190 230 280 340 410 490 580 680 790 910 1040 1180 1330 1500 1700 1920 2150 2400 2650 2900 3150 3400 3650 3900 4150 4400 4650 4900 5150 5400 5650 6000
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