EPS suggests a gradient pattern may develop over New England at the end of the run. I wouldn’t call it a SE ridge, but as the flow tries to relax with EPO ridge retrogression, the ridging develops a tad heading into Greenland. At the same time Canada is very cold. So verbatim battle ground is over New England towards the end. What you want to see is that ridging in Greenland take over and help pin the cold into eastern Canada. I’m not sure I buy that at the moment.