I feel like the models typically overdo the airmasses as we get into the transition portion of the season from winter to spring. They like to keep driving the deep cold thicknesses our way, but they are usually a mirage come verification time. This week is going to be a warm week for the northern CONUS and once we get a few days of that into the initialization I wonder if the models will start sensing more of the airmass modification with Tippy's cryosphere loss. Yeah, the cold is probably overdone either way because it's absurd anomalies so it's a moot point anyway.