Yeah obviously the development of any mesolow affects how quickly the drain accelerates from the northeast. In the Dec 2008 storm, a pretty well defined mesolow developed east of MA and into the gulf of Maine late afternoon and early evening of Dec 11. It accelerated the dewpoint drain into N MA and probably sealed the fate of all those lower elevation areas along and north of Rt 2 east of FIT and NW of 495....without that, they may have been more of a 32.5F rainstorm instead of a crippling grid failure type storm at 31F. Or at the very least...maybe more of a marginal ice storm without the heavier accretion rates that the drier air blowing in from the northeast helped enhance.