Figure 1 compares the prediction skill-scores of a set of numerical experiments with different initial conditions (IMAGE)
Caption
Figure 1. Spatial Anomaly Correlation coefficient that quantifies the capability of the model to represent the sea-ice evolution in three different set up: a) no initial correction (CTL); b) realistic initialization of surface field (SIR); 3) realistic initialization of surface and subsurface temperature and salinity (3DVAR). Red-dotted areas show regions where the sea-ice concentration is well predicted.
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Image by Morioka et al., Commun Earth Environ, 2022
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