-
Posts
7,099 -
Joined
-
Last visited
Content Type
Profiles
Blogs
Forums
American Weather
Media Demo
Store
Gallery
Everything posted by jbenedet
-
Those geese are still munchin’ away on green grass in Newington. They knew. But models!
-
That’s what I’m saying. The chances are up.
-
You want a make a cogent argument where a few degrees of warming has already made a huge difference in local climate—Buffalo NY. Lake Eerie open longer/later; slightly more instability with the warmer lake temps. These “anomalous” snowfalls will become much less so…
-
Very run of the mill cold here. 12/-1 DAW Eastport Maine with a forecasted high of 31. Have to head to Savannah Georgia to find temps that warm today. Pretty awesome.
-
Yea. Agreed. Lots of vulnerable spots in these areas. But if I had to pick most at risk it would be Portsmouth/Kittery at the mouth of the Piscataqua. I've seen the winds rip in this area with much weaker setups, but the severe conditions usually confined to right on the coast - inside rte 1A. This situation is obviously much different. Are there any good historical analogs?
-
Speaking for SNE - the lack of snow during this window from 12/1 to say 1/15, is most disappointing in terms of building a sustainable pack. Peak climo is later, sure, but the Solstice really does a lot to minimize pack reduction--it's difficult to overstate.
-
Subtle shifts, but the EPS has been trending towards an earlier/further south vertically stacked solution. It's shifted ~250 miles further south and east since 12z 12/20 runs. May not mean much in terms of the clown maps, but the current H5 depiction looks a lot more severe for Upstate NY, VT and western MA than 12/20 runs.
-
All criticisms aside, there will be some hell to pay for this level of UL forcing. The Southwest wind threat with the arctic front looks most threatening right now, overall. But the biggest threat looks like CT river West, where height falls are steepest. W CT looks most primed, where lapse rates are most unstable. Persistent strong southeasterly winds out ahead, off the relatively warm, moist Atlantic, set the stage.
-
She cuts off really early at 500 and 700; at the same time the surface reflection is ~1000 mb. I have always much less preferred such evolutions. Positive feedbacks between surface and UL's are greatly limited. Which is why the CCB snows (absent the LES enhancement) are so lame. The biggest snows occur when this thing is fully stacked and weakening; contrary to what we typically see. And that is in Ontario Canada, with widespread 12-24" amounts, which is certainly respectable. So the threat for a widespread heavy snowfall in the CONUS remains, but we need to see it fully vertically stacked some 500 miles further south than latest guidance.
-
Too much of a good thing: the arctic oscillation. With it so deeply negative any shortwave out west is “amp” happy. Deep cold is immediately tappable and synoptic wave development accelerates. Available cold is dumped west. We get the stale cold. Rinse repeat. Also explains why the best event for SNE ytd (sans the Berks) was that late blooming “crap” wave that barely registered 1000mb SE of the BM.