
eduggs
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Everything posted by eduggs
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1. Smaller events are usually shorter events and that means you might not be able to enjoy them due to work or sleep. 2. In places that don't get snow events very often, there can be a feeling like you have to cash in on every chance that you get because you can't count or another to look forward to.
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Yesterday's mid-Atlantic snowstorm had a ton of GOM moisture out ahead of the trof just pumping northward into a wall of cold air. We won't really have that luxury with this one. Here we need to rely on the dynamics of a rapidly deepening SLP and moist easterly inflow. The main precipitation shield is not likely to extend very far NW unless this really wraps up.
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You don't even have to look at the surface to see that guidance has shifted everything east. Look at H5 - best PVA is SE. The surface is just a reflection of the upper level divergence/convergence. Good thing is that if this sharpens up 10 %, the SLP ends up 100 miles NW. There will be plenty more changes.
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We're dealing with a little bit of a transition from the initial inland surface reflection and associated precipitation in PA to the developing coastal low. It's possible I-95 or just inland sees a bit of a precipitation minimum as the transition skips over this area and refocuses closer to the coastal. The precipitation shield as modeled looks to be shrinking and tightening as the SLP winds up.
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The heaviest precipitation has been modeled (GEFS, GEPS) along and south of I-95 for several runs with the heaviest in eastern NE. All major models have snow to the coast except the 6z NAM. So those graphics look a little funny. Ending at 12z Friday takes out most of what falls in NE. But I think those probs. heavily weigh members of the NAM model family...? Maybe the NAM is on to something. There is plenty of room for this to hook even further NW with a neutral tilt and vortmax in AR/MS by 0z Fri.
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As I clearly said, if you overlay the 80 hr GFS with the 84 hr NAM they are very close in most key features - unusually so. If you cannot concede that, you are being unreasonable IMO. The NAM does not have any more time to deepen. On NCEP, the GFS is 2mb deeper, 4 hours earlier, in nearly the same location. None of the rest of what you said makes any sense. It doesn't matter anyway, since we're 3.5 days out and it will change every 6 hours. I just think your original comment exaggerated a little bit.
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It's true we shouldn't be paying much attention to QPF at this stage. But this 36hr QPF image tells the tale of where a late developing coastal storm blows it load. Most would sign on for this type of outcome. Ensembles also give some indication of a higher ceiling. But let's not go crazy building up unrealistic potential based on the currently modeled features.
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All I'm saying is the GFS has almost the same negative tilt, same vmax placement, same jet core and positioning etc... which is why it develops a very intense SLP - low 960s or something - in the Canadian Maritimes. The NAM and GFS are not typically so similar 84 hours out. Maybe the NAM would go even wilder, but they don't seem so far off to my eye.
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If you overlay the 500mb vorticity chart of the NAM at 84hrs with the GFS at 80hrs, they look pretty similar considering the lead time. The NAM is maybe a touch sharper and there's more ridging both up- and downstream. But still very similar. So the GFS should be a reasonable estimation of what the NAM run might have led to. In this case, a deep and powerful storm in the Maritimes.