If the s/w ejects quicker, this would mean a higher possible chance of snow versus a CAD event since the S/W and the northern stream would be interacting with each other and the deeper colder air would still be in place(?) right?The 12z Euro improvements aren't surprising given that the trough over New England & Atlantic Canada is stronger and our s/w over the SW US ejects much faster this run, which again looks more like the patterns we saw in the more extreme & wintry 0z EPS solutions last night.
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