billski
Active member
Very good. This is when an inland runner triple points at just the right time (Its cold front catches up to the warm front, cutting off the moisture and begins to weaken the system) and transfers its energy to a secondary coastal low off of the Mid Atlantic. These are usually snowy systems for us. (Think December 27, 2013, that was a classic Miller B)
BE WARNED: When Miller B's are modeled this far out, they very well could become a cutting rainstorm if the transfer doesn't occur at the right time.
I think the only fair thing that can be said right now is, "that the pattern is very favorable for a large storm system to move out of the southern states." (stolen from AmericanWx)