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. 2024 Jul 30;14:17568. doi: 10.1038/s41598-024-63836-9

Figure 3.

Figure 3

(AC): mid February (left), April (center) and June 2013 (right) instantaneous snapshots of surface relative vorticity normalized at each latitude by the Coriolis parameter to visualize the local Rossby number Ro=|ζ|/f (the latitudinal band around the equator is removed). (DF): corresponding instantaneous snapshots of lateral divergence at the ocean surface. The black line represents the 250 m bathymetry line. The arrow on top of the panels (A,B,C) represent the average direction of the surface currents. The thickness of the line it is an indication of their intensity.