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Burghblizz

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Posts posted by Burghblizz

  1. Yinz are going to drive yourselves nuts clicking on hourly increments of hourly models for the 8 hours, and checking where the pretty colors line up. 

    I think E to W across central AGC will be the difference between 8 and 12 because of dry slot duration. And N to S along that axis will add or subtract ~2” from that range.

    Beaver /Lawrence/Butler certainly have a shot to pop a 15” total. 

    • Like 1
  2. Not sure how Tolleris is resolving the fact that the NW edge outside his sleet line is where the totals should ramp up - yet that’s where he has the totals drop off. Probably the single most important issue in terms of where big totals wind up.

    He tries to forecast for a wide area, and doesn’t put diligence into those areas. 

     

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  3. 11 minutes ago, MikeB_01 said:

     

    I just think this is where met intuition / experience comes in ahead of modeling. The discussions are full of comments about the rate of evaporative cooling. Even if we sleet, it should be brief and then we should be thumping again.

    I think this is why we all do well - but it’s like 5” to 12” well, as opposed to a nice tight range. 

    Where it’s ripping it will be ripping. Where it’s not, it might be a light mix for while, which will further hold totals down. So any prolonged period with that gets you behind the game.

    So a deeper storm hurts - because of the warm air aloft. But it also can HELP with dynamic cooling.

  4. 10 minutes ago, MAG5035 said:

    I do feel the same way, but I don’t completely discount the NAM’s robust warming higher up near  the 850mb level either. But same stuff as 12z. The money 3hr frames for ZR are 60 and 63. Using my nearest station at KAOO as an example since I’m in the thick of the heavy ZR over here.

    HR 60: Surface -6ºC, 925mb (~3k ft) -6ºC, 850mb +2ºC

    HR 63: Surface -2ºC, 925mb -3ºC. 850mb back to 0ºC

    Even with that basic breakdown at the major layers I look at that and ask what part of that suggests that particular station sees 0.78” as freezing rain? I think something toward a NAM scenario might get a few hours of sleet into the central and *maybe* western counties. But Pitt’s advantage is the 850 low tracks favorably on the NAM for western (and serviceable to central counties) plus overall flow is on the cold conveyor belt side of the low. We don’t have an Ohio Valley low with SW flow intruding in this situation and trying to overcome that with a secondary to the coast. The warm advection comes from the tremendous easterly flow aloft with the coastal low. I can’t really think of a situation in the past that has presented the NAM type scenario of that much mix/ZR into western PA so that would be a new one to me if it happened. 

     

    Thanks for your thoughts. He was weenying out a bit 

    • Weenie 1
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