Sea state with two wave systems traveling at oblique angles
Cross swell at Île de Ré, France. The waves themselves are examples of cnoidal waves.Cross sea near Lisbon, Portugal.
A cross sea (also referred to as a squared sea or square waves[a]) is a sea state of wind-generated ocean waves that form nonparallel wave systems. Cross seas have a large amount of directional spreading.[1] This may occur when water waves from one weather system continue despite a shift in wind. Waves generated by the new wind run at an angle to the old.
Two weather systems that are far from each other may create a cross sea when the waves from the systems meet at a place far from either weather system. Until the older waves have dissipated, they can present a perilous sea hazard.[2]
This sea state is fairly common and a large percentage of ship accidents have been found to occur in this state.[3] Vessels fare better against large waves when sailing directly perpendicular to oncoming surf. In a cross sea scenario, that becomes impossible as sailing into one set of waves necessitates sailing parallel to the other.[4]
A cross swell is generated when the wave systems are longer-period swells, rather than short-period wind-generated waves.[5]
^Toffoli, A.; Lefevre, J. M.; Bitner-Gregersen, E.; Monbaliu, J. (2005). "Towards the identification of warning criteria: Analysis of a ship accident database". Applied Ocean Research. 27 (6): 281–291. doi:10.1016/j.apor.2006.03.003.
