What the hell is this 
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Naughty November
- Thread starter LickWx
- Start date
What the hell is this
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Is that a freaking squall line????
I think I saw Nashville gusted to 53 with it
Usmeagle2005
Member
It packed quite a punch in Tupelo for like 30 seconds.? went from noting to blinding rain and wind back to nothing it that time.What the hell is this
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Paging bird
Interesting gfs run incoming 
I hope I'm wrong, but too far NW. ?
Yeah probably gonna be a Wilkes onset ice run, hey at least there’s a solid pattern showing up around this time
I think that's a bit too optimistic, would be a storm for maybe Mack. However, I do think there is an obvious trend in the high pressure/cold air source. Now we need to work on timing and making the west coast look better.
Yeah I’ll take this trend of a slower trough in SE Canada
Looks like perfect location! ?
That’s a hell of a high pressure, but even I rain!?
Meanwhile you got the CMC showing severe weather, lol 
Not 0 right modernweenie
Tis the season. November always offers up those low cape/high sheer severe weather events. Although, with it being 2020 and La Niña I bet you get one or two significant ones.
Webberweather53
Meteorologist
Webberweather53
Meteorologist
Long, longgg ways to go but we definitely have the right longwave pattern to crank out a Miller B/CAD event around or just before Thanksgiving and that's all you can really ask for 10 days out.
Deepen the trough over Atlantic Canada and the surface high over New England will trend stronger & "lock in". More Atlantic Canada troughing implies more cold advection in New England (therefore a stronger surface high) & deeper troughs move more slowly as they experience more planetary vorticity advection (thus, the surface high doesn't leave as quickly). These setups can easily change pretty dramatically even inside day 3-5 so plenty of time to watch it. Also will need a properly timed wave to emerge out of the southern Rockies before this Atlantic Canada trough leaves stage right
Deepen the trough over Atlantic Canada and the surface high over New England will trend stronger & "lock in". More Atlantic Canada troughing implies more cold advection in New England (therefore a stronger surface high) & deeper troughs move more slowly as they experience more planetary vorticity advection (thus, the surface high doesn't leave as quickly). These setups can easily change pretty dramatically even inside day 3-5 so plenty of time to watch it. Also will need a properly timed wave to emerge out of the southern Rockies before this Atlantic Canada trough leaves stage right
Snovember weenie-ing aside, 12z euro was damn cold in its last frame
