It's tough too because the ocean is pretty vast, good ocean/lake effect needs land nearby to focus the lift within one or two dominant bands. That's why this is performing so well. LI/CT shores are confining the band to its current location and it just waffles with the wind direction.
But in big arctic outbreaks you see the streamers from cold air pouring off the continent but they rarely organize into single dominant bands, they organize into smaller convective rolls. You can get some that are more dominant, but usually because they originate from a water feature bounded by land (Penobscot Bay, NY Bight, Narragansett Bay, etc).
There's a reason the LES from Lake Michigan is more potent on a north wind vs. a west wind, and it's not just the longer fetch. The band parallel to the land features is just more focused.