Makes sense. In this case trajectories are more towards the N/NE, instead of veering east with a squall line racing well east…That’s when we run into more of an issue. In this case the N/NE trajectory will cause an overlap of some convection making it into the cold sector, which is why we have that narrow axis of ‘higher’ snowfall accumulations being possible. Without it, deformation axis snows are lower end. .