That’s a stout -epo, I think cold could really dump hard into conus week 2.
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You know, this kind of hit me earlier today as I was watching a model run.
One of the key rules with wave breaking within jet streams is that if the jet is running more poleward (farther north), it's more likely that the waves are going to break anticyclonically (rollover to the right at the top of the ridge)...while when the jet is running more equatorward (farther south), it's more likely that the waves are going to break cyclonically.
La Nina is associated with more poleward jets / more anticyclonic wave breaking (on average) / El Nino is associated with more equatorward jets / more cyclonic wave breaking (on avg, especially later in winter). So, we can see a good example of that now in the North Pacific. What this means is, as that ridge climbs up into AK, it's less likely to break anticyclonically, which is what you would want to see to get more cold air sent south. Now, I'm not saying that we can't get cold air sent south, but those are some ideas associated with the setup here. Some of the model runs do have some level of anticyclonic wave breaking atop that ridge, but not in a bold way. Also, you could have a ridge-bridge type deal where the AK ridge runs head on into the Greenland Blocking ridge and that could dislodge some cold as well. So, we'll probably need to rely more on the setup of the Greenland Block / 50/50 low / Surface High Pressure over the Great Lakes to deliver the cold south.
This concept of anticyclonic and cyclonic wave breaking makes me think of some other related things:
1. On that first image I posted, you can see how La Nina-like anticyclonic wave breaking over Alaska could easily lead to a -PNA pattern. In contrast, you can see how the El Nino-like cyclonic wave breaking in the Pacific leads to waves breaking off the Aleutian Low and them tracking east into California and Baja, while also leading to western ridges that rise up the U.S. and Canada coastline (negative tilt)
2. On the Atlantic side, you can see how cyclonic wave breaking is preferred for the development of -NAO because after the ridges climb north, they will then move west, feeding into the development of the Greenland block