“…It is well-known that the flow beneath a rotational water wave with constant vorticity is characterized mainly by: i) the appearance of stagtnation points -fluid particles with zero velocity in the wave's moving frame; ii) critical layers -a horizontal layer with closed streamlines separating the fluid into two disjoint regions; iii) the arising of pressure anomalies such as the occurrence of maxima and minima of pressure in locations other than below the crest and trough respectively. These results have been showed numerically [5,27,29,30], asymptotically [3,20] and also proved rigorously [14,33,24]. The constant vorticity also affects the shape of the free surface, for instance its profile can become rounder and possibly form an exotic overhanging wave [31,32,9,10].…”