Li, Y. W., and Coauthors, 2020: Eddy-resolving simulation of CAS-LICOM3 for phase 2 of the Ocean Model Intercomparison Project.. Adv. Atmos. Sci., 37(10), 1067−1080, https://doi.org/10.1007/s00376-020-0057-z.
Citation: Li, Y. W., and Coauthors, 2020: Eddy-resolving simulation of CAS-LICOM3 for phase 2 of the Ocean Model Intercomparison Project.. Adv. Atmos. Sci., 37(10), 1067−1080, https://doi.org/10.1007/s00376-020-0057-z.

Eddy-resolving Simulation of CAS-LICOM3 for Phase 2 of the Ocean Model Intercomparison Project

  • A 61-year (1958–2018) global eddy-resolving dataset for phase 2 of the Ocean Model Intercomparison Project has been produced by the version 3 of Chinese Academy of Science, the State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics/Institute of Atmospheric Physics (LASG/IAP) Climate system Ocean Model (CAS-LICOM3). The monthly and a part of the surface daily data in this study can be accessed on the Earth System Grid Federation (ESGF) node. Besides the details of the model and experiments, the evolutions and spatial patterns of large-scale and mesoscale features are also presented. The mesoscale features are reproduced well in the high-resolution simulation, as the mesoscale activities can contribute up to 50% of the total SST variability in eddy-rich regions. Also, the large-scale circulations are remarkably improved compared with the low-resolution simulation, such as the climatological annual mean SST (the RMSE is reduced from 0.59°C to 0.47°C, globally) and the evolution of Atlantic Meridional Overturning Circulation. The preliminary evaluation also indicates that there are systematic biases in the salinity, the separation location of the western boundary currents, and the magnitude of eddy kinetic energy. All these biases are worthy of further investigation.
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