I'm posting from my cell phone this morning just to get some thoughts out quickly:
First, I see nothing that indicates the going forecast is in jeopardy for blizzard conditions in the higher terrain of Northern New England. I think yesterday's thought-process holds and this post is meant to supplement, not replace that thinking. I see continued reason to pay careful attention to a possible phase change in Central NewEng, especially Northern MA to Southern ME.
Mid-level center has excellent radar presentation well S of NewEng over open waters. Tropical tap of moisture has commenced ad is responsible for blossoming precip shield. This is all evidence that the ingredients have successfully come together for rapid cyclogenesis as a "bomb" develops right along the NewEng coastline.
This continues to be a dynamically driven event. The major players are found aloft, not at the surface, and that's part of what makes the forecast a bit tricky, because there is no well defined surface based baroclinic zone you can key in on for phase changes (rain vs snow) or storm track. That said, the cold pool aloft is impressive an through ageostrophic flow and dynamic cooling, the storm develops it's own baroclinicity from the top down.
There's still a notable absence of antecedent cold air evident on the surface plot this morning, but stations like St. Johnsbury are 34/32 and this is evidence an elevation event is in the cards. While snowfall amounts will increase markedly above 1000 feet, I do think that all but the deeper valleys of Northern NewEng should squeeze out a couple of sloppy inches, at least, with dynamic cooling overcoming the warm bubble of air that remains trapped in the lower elevations.
I see no reason to deviate from blizzard conditions in the higher terrain above 1000 feet, when cold advection favors downward momentum transport and the increasing ageostrophic flow cranks winds to 50 knots at 850 mb overnight Fri night into Sat AM and we mix that down for several hours of 45+ mph gusts.
There are still two areas of greatest uncertainty. The first remains in Central and especially Western Maine, including Portland, Augusta and Sanford, even into Rochester and Stratham NH. Myconcern here is continued evidence that the end of the period of most rapid intensification just off the Maine coast pulls down a small tongue of cold air from the mountains, with origins in Eastern Canada. In an already somewhat marginal environment and with such intense vertical ascent due to dynamic lift in the comma head precip, I'm actually expecting to see a burst of "surprise" heavy snow sometime the first part of Friday night, with changeover starting not long after sundown. Accumulations would be unlikely to exceed a couple of inches of wet snow, and it may appear in pockets beneath only the greatest upward vertical motion.
Finally, there is the question of Southern NewEng. Temperatures are far less marginal here when the strongest dynamic lift come through, so the potential for a meaningful surprise event is smaller. Still, as mentioned in the streaming technical discussion, north of the MA Pike the precip will be more stubborn to shut down and the cold air advection kicks in, so by Friday night, there is the potential for some light snow from the Worcester Hills to Southern NH/MA border, still thinking in pretty much the same area indicate on the accumulation map that appears in yesterday's video TV forecast, in the post below.
That's all from me for now. Going to be a great storm to watch. Have you tried the Google Earth radar linked at the top of this page yet? I think you'll like it.
Matt