Z
Zander98al
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How does further west effect the southeast? Does it make it more likely for negative tilt when it moves northeast? For snow on the northwest quadrant of the low?View attachment 110197
NAM is further west as well
How does further west effect the southeast? Does it make it more likely for negative tilt when it moves northeast? For snow on the northwest quadrant of the low?View attachment 110197
NAM is further west as well
This is a really good discussion. I know this probably gets overused a lot but the whole data sampling is definitely important with a set up like this. When it comes to phasing, being off by just a few hours can have huge implications to what actually verifies. I forgot who, some one earlier today brought up the comparison with what models are showing right now to March 1980, March 1993, and January 2000… while I was too young to remember March 1980, I do remember that with both 3/1993 and 1/2000 being off on phasing by a matter of hours very much effected what was forecasted and what verified.RAH still watching. Might be looking at 0z runs tomorrow night before models align better.
Friday and Friday night: The upper trough over the central and
eastern US will reload as yet another strong, amplifying shortwave
trough dives SE, reaching the SE US late Friday/early Saturday.
Models keep any coastal low pressure system development offshore,
just how far offshore remains high uncertainty and remains a source
of large model spread in just how much liquid equivalent precip will
occur inland. Given that the shortwave trough in question is still
in a data sparse region over the Gulf of Alaska, expect to see a
narrowing/clustering of solutions once the system moves onto the NW
Pacific coast within the next 24 to 36 hours. Based on current model
projections, precip should begin as all rain with critical onset
timing occurring after daybreak Friday. If inland
precipitation/moisture is adequate, precipitation type could change-
over to snow Friday evening/night before ending from deep column
cooling as the northern stream trough moves into the area.
All the players should be on the field for data sampling by Wednesday ?This is a really good discussion. I know this probably gets overused a lot but the whole data sampling is definitely important with a set up like this. When it comes to phasing, being off by just a few hours can have huge implications to what actually verifies. I forgot who, some one earlier today brought up the comparison with what models are showing right now to March 1980, March 1993, and January 2000… while I was too young to remember March 1980, I do remember that with both 3/1993 and 1/2000 being off on phasing by a matter of hours very much effected what was forecasted and what verified.
This is a really good discussion. I know this probably gets overused a lot but the whole data sampling is definitely important with a set up like this. When it comes to phasing, being off by just a few hours can have huge implications to what actually verifies. I forgot who, some one earlier today brought up the comparison with what models are showing right now to March 1980, March 1993, and January 2000… while I was too young to remember March 1980, I do remember that with both 3/1993 and 1/2000 being off on phasing by a matter of hours very much effected what was forecasted and what verified.
Model integrity has improved, but we’re still talking about phasing which is still something very difficult for even today’s models to nail down to the detail. The computers need as much data as possible to come out with the most accurate solution… I’m honestly suprised that NOAA isn’t sending out some air craft to the Pacific on this one with number of people a potential storm could effectHasn’t model integrity improved since those storms?
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Not at allI'm guessing with the energy dropping more to the Southwest. That means like a pendulum it'll make it move Northeastward sooner? Through far eastern panhandle and southern Georgia?
Of the many different ways storms can amplify, one is for it to dig further west to allow more time for it to develop.Not at all
Wave packet dropping down thru the Rockies just split…one to the Ohio Valley and another to Arizona. GFS pulled that move some with the last storm before correcting late. CMC was doing this a couple days ago tooWasn’t the euro showing something similar last night though? Super flat?
Yeah I think we’re still at a point that we’re gonna see different solutions. Ultimately I think Wednesday as the data sampling is better is when we’ll see a solution form. There is just so many moving parts with this set upWave packet dropping down thru the Rockies just split…one to the Ohio Valley and another to Arizona. GFS pulled that move some with the last storm before correcting late. CMC was doing this a couple days ago too
That may be better than the last run. That's rain for you, though, buddy!JMA is the scenario most of us want. We need the southern energy to phase and come out.
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It's not really ots though. It's sheared out which is really bad if we want the energy consolidated at the base of the trough in order to amplify quicker.Personally I think the gfs looks about how you’d want it to at this point, for this to work out for anyone south of Virginia we need to keep this ots for as long as possible
I wouldn’t be too drastic about it .. it’s more like a step in the wrong direction knowing we have 100 hours to step back in the right directionGEFS was way worse
That’s a big snow for us on the JMA! ?That may be better than the last run. That's rain for you, though, buddy!
And the GFS is allowed one bad run. It needs a break. It's probably tired from whipping the Euro all over the place this winter.

We have a clear target…day 3 or so we will see if models converge or diverge from that energy coming out. Let’s hope RGEM shows that tonight or into tomorrow.I don't see the big cause for concern. Both/all waves are really still stuck in their parent trough/vortex somewhere north/south of AK. Let's at least save the freak outs until they become their own identifiable features that can be initialized.