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January Storm Term Threat Discussions (Day 3 - Day 7)


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Just now, psuhoffman said:

If this fails the lingering of the early week system which decreases the spacing and prevents ridging from really going up behind it is probably the biggest culprit. It’s the biggest change in the overall pattern from when I looked at it a week ago and really like it. The spacing isn’t as good now. Of course as the system approaches we are barely on the cold side and temps crash as the coastal forms...so whose to set had ridging gone up more this doesn’t cut and jump to the coast too far north like a lot of the gefs members that rained on us the other day. Our “win zone” with every storm is so narrow with the current temperature profile.  

I’d also think that traditionally, with a low as strong as the GFS is depicting moving across southern Virginia it would create a larger shield of snow on the north side. 

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The gfs and the para looked different on all runs leading up to this point with the para being the best for most of us, but they don't look to be that far apart anymore.  Thursday is still a storm and four days away, so I'll keep watching but the para is definitely more in line with the other more south models.

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5 minutes ago, Maestrobjwa said:

Is it such a terrible spot to be in 4 days out, though? Still looks close to me...

No this setup is bleeding the wrong way. Has been for the last several days honestly but somehow the gfs continued to amplify the h5 way more then all other guidance anyways. But the trough in front is slowing down more and more, that tpv in Canada is diving south more each run and the combination is compressing the flow a lot more. Frankly had the h5 flow looked the way it does now when I got excited 10 days ago I probably wouldn’t have. Imo the bigger failure is the wave Monday.   The progression sped up. That wave is happening during our best window wrt the Rex block and trough retrogression. But frankly the pathetic lack of cold F’d that up. No nice boundary for the wave to focus along, and that’s hey because it’s a surface driven not upper level wave.  So it’s  washing out and we weren’t even cold enough anyways if it hadn’t to maintain heavy snow.  But simply from a pattern progression that was our best shot to get a simple overrunning snow in DC.  The timing has changed for the next wave. The trough amplifies too much off the east coast and the ridge stops retrograding behind it. The wave after has a better chance to amplify but by then what pathetically little cold there is has eroded even more since the polar source is cut off. Imo the root of the fail was we had 5 days of epo ridge that opened a direct air feed off the Arctic straight down into southern Canada and the northern US...but that air quickly modified and mixed to become just an average blah airmass. That limited the potential of EVERY discreet threat within the blocking window.  Created the double bind. Less potential energy from a weaker boundary. Made us need more suppression to stay cold. But less likely to get amplified waves.  It’s not 100% over. Weirder things have happened. But I’m past the point of expecting it. 

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Unfortunately in this case the upper level pattern is trending unfavorably for our latitude. The 500 ridge out west is setting up too far east over the Plains where ideally it should be over the western states. Upper level low over southern Canada with the high nosing leads to a more progressive and southern system. The 500 energy comes at us more west to east vs a larger cutoff feature given the pattern. Unless we see changes to these features, the southern/progressive/slider type of a system would continue.

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12 minutes ago, chris21 said:

I’d also think that traditionally, with a low as strong as the GFS is depicting moving across southern Virginia it would create a larger shield of snow on the north side. 

Less cold less resistance to WAA less lift less healthy precip shield to the north. We’ve seen that all year with every wave. The path to overcoming that here was when it was an extremely amplified bomb. It’s a balance. A weak wave with a weak WAA flow can create lift by having a deep hard to move cold airmass that resists the WAA creating lift. With less cold you need the flow from the wave to be stronger to compensate. Of course that opens the door to rain lol. See!  

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