The northern stream digging more is just such a fantastic trend. I think that if you're scratching your head about this (hey, I thought a stronger, more amplified shortwave would be warmer!" it's completely understandable because that's how most of our events work. Last weeks system was a pretty good example of this- we're pretty used to amplification of our shortwaves causing more warm air advection and the system to achieve negative tilt sooner. However, the location matters- last week's amplification trend took place around arklatex- so yeah, it makes sense as that trough got stronger, the ridging ahead would also get stronger.
For this system, as the northern stream gets stronger, it's digging much further south, and generally depressing heights for the wholesale region because of how much more it is digging. I think that's why snow totals have actually ticked SE over the last cycle. Sure, as this feature gets stronger, the processes like WAA get stronger as well. The southward shift is doing a good enough job to shunt these forces southward a well. The northern stream shortwave as it turns out did detach from a much colder longwave trough, so it makes sense that as it digs southward, that chilly arctic air hangs on a little longer.
(BTW, in case anyone is wondering why an account with like 20 posts over 4 years is now writing a dissertation on phasing, I've lurked here for a while. I originally got on here to troll a friend of mind who now happens to be banned. But I still stay on because I enjoy the expert GIF makers on here and the pay graphics that get posted. I'm typically more active on American under the name "ILMRoss")