This type of Hudson Bay / James Bay Vortex pattern isn't the best at producing highs over the Great Lakes and Northeast with a 50/50 low. However, when the trough is established across the conus, it can be a good mechanism for getting storms to track across the south with cold air in abundance lurking to the northwest.
Here's an example storm that did work out in this type of pattern from New Years Day in 1962.
Storm Totals were:
Atlanta: 1.0
Gainesville, GA: 5.0
Charlotte: 6.0
Asheville: 6.9
Greensboro: 6.6
The wave/sfc low are off the British Columbia coast at the start of the loop...