I always remember Shane saying over the years that while we hate the SER, you also need a little ridge to keep winter storms from missing altogether. Perfect example right here
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I always remember Shane saying over the years that wile we hate the SER, you also need a little ridge to keep winter storms from missing altogether. Perfect example right here
Very nice.Slight improvement and the big takeaway is it stopped any eastward shift, 0z and 06z below, definite shift west (again slight but still positive)
edit: shift west but also lighter amounts in some locations
His maps are indeed extra. But I respect it. If I had to wager, I thought his totals actually might have been a little lower in the Triangle area. 11th hour is approaching.Makes me laugh a little bit about how complicated it is to forecast winter weather in the SE. Hats off to those who try!
Quite the shift NW the past 2 hrrr runs View attachment 108677
Where the hell is the wave at?! This thing is go time for tomorrow lmaoI'm not a huge believer in wait until the wave gets sampled I think it falls into weenie lore but I would certainly feel better if we had all pieces over the US at the moment for the 12z runs. It's such a small change required to make a relative large change at the sfc it bothers me with this one. I really don't trust a meso model ATM if they are blowing it at 500mb the sfc features are pretty irrelevant
I always remember Shane saying over the years that while we hate the SER, you also need a little ridge to keep winter storms from missing altogether. Perfect example right here
This one is really on the edge of a knife. I agree, I think it matters somewhat in this instance. I also think it matters in the 2-5 day time frame too, depending on the orientation and nature of the general 500 mb longwave pattern. I think it plays a significant role in why we often anecdotally recognize storms "disappearing" during that window and reappearing as we get closer. But for the most part, it's overused and just randomly tossed out as if it's universally applicable in every situation, like so many other things.I'm not a huge believer in wait until the wave gets sampled I think it falls into weenie lore but I would certainly feel better if we had all pieces over the US at the moment for the 12z runs. It's such a small change required to make a relative large change at the sfc it bothers me with this one. I really don't trust a meso model ATM if they are blowing it at 500mb the sfc features are pretty irrelevant
Almost identical to the 0z EPSWhat did the 6z euro eps look like?
This one is really on the edge of a knife. I agree, I think it matters somewhat in this instance. I also think it matters in the 2-5 day time frame too, depending on the orientation and nature of the general 500 mb longwave pattern. I think it plays a significant role in why we often anecdotally recognize storms "disappearing" during that window and reappearing as we get closer. But for the most part, it's overused and just randomly tossed out as if it's universally applicable in every situation, like so many other things.
That s/w you've been mentioning, I guess the 3rd piece of the puzzle, that trails and could sharpen our wave a little more is the one that hasn't been sampled yet correct? Would stronger be better for that one?I'm not a huge believer in wait until the wave gets sampled I think it falls into weenie lore but I would certainly feel better if we had all pieces over the US at the moment for the 12z runs. It's such a small change required to make a relative large change at the sfc it bothers me with this one. I really don't trust a meso model ATM if they are blowing it at 500mb the sfc features are pretty irrelevant
That s/w you've been mentioning, I guess the 3rd piece of the puzzle, that trails and could sharpen our wave a little more is the one that hasn't been sampled yet correct? Would stronger be better for that one?
Yeah the more energy you can drop into the base/back of the current trough the more you can attempt to slow it down, dig it, tilt it. That means downstream a more amplified divergent jet, higher coastal heights, more waa/fgen/isentropic lift aloft.That s/w you've been mentioning, I guess the 3rd piece of the puzzle, that trails and could sharpen our wave a little more is the one that hasn't been sampled yet correct? Would stronger be better for that one?
Ok maybe so. I’m putting a little more credibility on globals at this moment, although starting at 0Z will definitely give mesoscales more weight.This HRRR run is kind of what I am thinking, dusting to an inch back to Wake County with 2-3" in far N/E NC.
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Hour 30 is a nice tick NW vs previous run. This is much better at 5h and precipitation and 7h is responding.doesnt get it done, ugh. out of time im afraid.
Whish one is correct and when will we know? Looks like not until about 1pm ET tomorrow for which perturbation will actually be correct6z GFS v/s 12z NAM. This is the difference between a whiff and 3-4" for many in central/eastern NC
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