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Winter model mehhem or mayhem nature will decide


weathafella

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The cluster analysis is definitely not showing any model camps yet. There are certainly clusters of ensemble members, but each cluster includes CMC, GEFS, and EPS members. So it's not a North America vs. Euro situation.

The cluster we want (stronger western low and slower) is definitely the farthest west with the trof, stronger southern stream, and more Atlantic ridging. The western ridge doesn't seem to be a significant driver, because that cluster is in the middle of the pack regarding heights.

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2 minutes ago, OceanStWx said:

The cluster analysis is definitely not showing any model camps yet. There are certainly clusters of ensemble members, but each cluster includes CMC, GEFS, and EPS members. So it's not a North America vs. Euro situation.

The cluster we want (stronger western low and slower) is definitely the farthest west with the trof, stronger southern stream, and more Atlantic ridging. The western ridge doesn't seem to be a significant driver, because that cluster is in the middle of the pack regarding heights.

so baby steps........?

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1 minute ago, 512high said:

so baby steps........?

More showing us what we need to be paying attention to.

It is good that the majority of the ensemble variance is related to the low pressure (stronger vs weaker, slower vs. faster) instead of some other feature in the flow. So changes to the features I mentioned will drive changes in the low pressure. For instance, right now over 50% of the ensemble variance is in the strength of the low off New England. That's pretty high for day 5/6.

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2 hours ago, jbenedet said:

These sub 960 members off the SNE coast aren’t unrealitstic imo, given the airmass over the northeast is typical of areas 500 miles to the north. Usually it’s SE Canada that gets the nuke, but we are in SE Canada right now, if you will....

This is a great point!

Not so much because we (or at least "I") am willing to advertise a cyclone capable of peeling the Earth's lithosphere right of the mantle like that...

BUT, pragmatically to the science of Meteorology?  The idea of these ridic cold air masses sitting idly by one of the greatest warm conveyors known to the planet for so long, without a consequence, is a pricey request. It is a circumstance so fraught with potential that it truly is understandable that an "option" or two in a perturbed model suite of plausible outcomes might actually ..oh, gee,  pick up on that sort of thing.

Anyway... for the general reader: Bomb or not, the fast flow is still a problem for "maximizing" impacts.  If mega bomb moving along at ludicrous speed will be severe for a comparatively less amt of time and thus limit therein.  There's probably a reason why super deep lows don't tend to stick around that often ... because they have to be drilled into a planetary wave response to derive their mechanical might.  Another reason why years like 1978 (or any not named) are pretty fantastically rare.   

 

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