Excellent question! There's been during the 6-10 day a tendency for too much W US ridging along with too much E US troughing thus leading to a tendency for the E US to be too cold and some of the west being too warm. In essence, a good bit of this is the SER being badly undermodeled just as was the case last winter. The Maxar met (who is very smart and knowledgeable), as you'll see below, says that is still an E US "cold bias". But on top of that there actually has also been a same day cold E US bias. Here's this Maxar met's response to me, which was a reply to my asking the same Qs you asked as I wanted to make sure I wasn't mistaken in calling having too cold a pattern in the E US a "cold bias":
"Hi Larry,
Cold bias is used to reference the model being too cold versus reality. This could be for varying reasons, including a simple miss in the pattern (arguably what we see in longer range projections). Here is an example using the current 6-10 Day maps comparison to when the period was in the 11-15 Day period (note the Southeast ridge in the more recent runs compared to troughing when in the 11-15 Day):
That said, the model has also been too cold in its same day projections (i.e. morning projection for the day of), so some bias even when the larger scale pattern is figured out.
I hope this helps. Let us know if you need anything else."