 This environment would produce large amounts of crosswise vorticity (via the right hand rule, vorticity with an axis of rotation perpendicular to the environmental flow).As an updraft begins to form, it will tend to tilt the crosswise vorticity lines into the vertical, resulting in an anticyclonic vorticity axis on the northern fringe and a cyclonic vorticity axis on the southern fringe of the updraft.At this point, despite vorticity lines being oriented in the vertical, the storm "can not" be considered a supercell, as the areas of rotation are "outside" of the main updraft.