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Assimilation of HF radar surface currents to optimize forcing in the northwestern Mediterranean Sea

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Figure

Figure 1. Depiction of the studied area. The larger area is the model domain (MD). Red points mark radar stations PEY and BEN
Figure 2. Hovmöller diagram of radial velocities from the PEY station along a south–north transect at 6.2simulation and◦ N (see Fig
Figure 3. Schematic representation of the optimization window(winana), the backward (win−obs) observation window and the for-ward (win+obs) observation window
Figure 4. Root mean square error Er time evolution ofover the POD (full lines) or the MD (dashed lines)
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