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Northeast Montgomery may need a tornado warning soon.
Pattern for next week appears to be unraveling with the trough not phasing properly and one of the shortwaves feeling the weakness from the TC in the eastern Pacific. Leads to much less flow over the Plains.
1816 is that you???Looks like a big a$$ shot of anomalous cold air coming down from Alaska, bringing snow to portions of the Rockies. Then, causing a strong 20 degree temperature swing between the two air masses in the plains. Is it abnormal to be getting an arctic blast like this in June?
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Well there was what looks like a confirmed spin up tornado in Henry county like 20minutes ago that had a debri signatureFirst day in what feels like forever that there isn't an MCS ongoing over the Southeast. Still feels like soup out there, though.
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Do you mean effective shear values? Because I would definitely not call anything above 200 m2/s2 of 0-3 km SRH low shear (I see some >400 m2/s2 soundings in here too?) Maybe for violent tornadoes 200 m2/s2 is a little low, but that's still adequate for tornadogenesis.Went through my collection of soundings and found some June low-sheer tornadic events. Low sheer June tornadoes are pretty common in Montana, Wyoming, Colorado, and the Dakotas.
Barnard, SD EF4
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A photogenic F3 with 5 other tornadoes in Kansas. 06/13/2004.
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An EF4 tornado and the largest outbreak on record for Minnesota. 2010 had 5 June tornadic events.
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Massachusetts long-lived EF3 in 2011
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"cold-core" outbreak in the Northern Plains. 2011
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The Pilger, NE twins. 2014.
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Photogenic South Dakota EF4. 2014
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A simultaneous cyclonic and anticyclonic tornado in Colorado. 2015.
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Higher sheer, but the most notable June tornado of the last few years.
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Kansas tornadoes and mothership supercells
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Additionally, there haven't hardly been any June outbreaks in the plains in the last 10 years, and most of the meanest June tornadoes in the plains occur with 60-80 kt eff sheer. When sheer gets that high, June tornadoes get especially violent. With several large outbreaks and EF4s.
I believe the 250ish range and above tends to be the sweet spot for SIGTORs, but don't quote me on that. That said, tornadoes can occur even in pretty pitiful SRH values, and summertime tornadoes can often kinda defy typical expectations for kinematics.Do you mean effective shear values? Because I would definitely not call anything above 200 m2/s2 of 0-3 km SRH low shear (I see some >400 m2/s2 soundings in here too?) Maybe for violent tornadoes 200 m2/s2 is a little low, but that's still adequate for tornadogenesis.
I'm talking about effective shear yes. SRH is storm relative helicity. Is that considered a form of shear too, because I thought they were separate things? I also thought 500 mb winds were sheer, and that's the biggest question mark with next week. I must be misinterpreting. 500 mb winds and low level jets are admittedly my weakest area of understanding.Do you mean effective shear values? Because I would definitely not call anything above 200 m2/s2 of 0-3 km SRH low shear (I see some >400 m2/s2 soundings in here too?) Maybe for violent tornadoes 200 m2/s2 is a little low, but that's still adequate for tornadogenesis.
Yeah, I've heard of the outbreak Jarrell was involved in being a prime example of this. Pitiful low level kinematics, but the storm responsible for Jarrell was located at the cusp of the dryline "zipper" with the cold front to the west and stationary front to the north. That and the fact that there were many other tornadoes that day, including another violent one rated F4, which is very interesting.I believe the 250ish range and above tends to be the sweet spot for SIGTORs, but don't quote me on that. That said, tornadoes can occur even in pretty pitiful SRH values, and summertime tornadoes can often kinda defy typical expectations for kinematics.
It's totally understandable to misinterpret this, but yeah, SRH is considered a part of wind shear. Effective shear is technically a different thing, and all I know about it is higher values of effective shear are better for supercellular development/storm development in general. I think it also plays a role in how large supercells for a certain event may end up being. I could be wrong on this because I'm not a met, but I believe effective shear is basically the wind shear through the entire altitude of the atmosphere, while SRH is wind shear measured in the lower levels - at least that's my way of understanding it.I'm talking about effective shear yes. SRH is storm relative helicity. Is that considered a form of shear too, because I thought they were separate things? I also thought 500 mb winds were sheer, and that's the biggest question mark with next week. I must be misinterpreting. That's admittedly my weakest area.
What the heck is the deal with this area of GA lately?
Central Georgia has the sand moutain effect lolI feel like in the same way North Georgia has magical anti-tornado qualities, Central Georgia has like... the opposite.