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That might actually the lowest modeled thickness I've ever seen. 474mb over Lake Superior/
If only we could get a cyclone to spin up in the gulf. Would be an absolute unit.
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Bouncy is this a concern? Or we heading to another storm like we just had this weekend??If only we could get a cyclone to spin up in the gulf. Would be an absolute unit.
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Appears to reconnect later in the run.. This run may be a huge dump of snow.
snow for ATL first...then a sleet maker...I think!Snowing from New Mexico to Bermuda View attachment 185369
multiple impulses?Snowing from New Mexico to Bermuda View attachment 185369
Yeah I don't know that I've ever seen something like this, even in fantasy range. And I'm not even just talking about the surface/snow.. just the meteorology of it all. The never-ending overrunning followed by cyclogenesis attempts off the SC coast AND the Texas coast at the same time, just prolongs the moisture fetch under a tank of a banana high.This might be an all time stupid GFS run if it can hold
The weird thing is, do you even see this as an impossible scenerio? I feel like if you get a general overrunning setup with a high pressure that strong, it could be a legit risk in an extreme scenerio. This is something we need to monitor extremely closely. Could be an outlier run.
Snow from NM all the way to NC with some ice even down into MEXICO. This is crazy
Idk how this can even be possible. And it’s not the only model that has shown it this way. But I’ve never seen it so my gut just tells me it can’t happen like that.
Reason why the AIGFS sucks is because it’s to elongated with the TPV appendage, and that boxes us in with warmer air, and disrupts the cold feed. Not to concerned given nothing else showing if but it’s in the back of my mind, sometimes these TPVs don’t play nice View attachment 185366
My eyes always light up when I hear "split flow". My best storms have been in a split flow, and often back to back. Get the cold air in place, and stubborn, and the impulses keep riding in.Split flow for the win. I noticed that a large portion of the biggest SE winter storms had a split flow H5 signature with moist WSW H5 flow for the subtropical jet underneath moving in tandem with a cold NW flow of the polar jet directly to its north in the Plains states.