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Everything posted by jbenedet
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It's subtle but the GEFS trending towards other warmer guidance the past 2 model cycles. The WAR hook-up that we have seen so often this season, with confluence in place. This translates to much more of an easterly fetch despite the Canadian high in a good spot (initially). The cold canadian dews fighting the dews advecting off the atlantic.
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I don't disagree. But again, to my original post "equal chances" in mid march, New england, is far from hostile.
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We're after accumulating snow. that's one point. Not necessarily profiles that support snow. The other is - HP/LP it's all relative. Will the cold win? Well it's surrounded by relatively warmer air. Cold is on the run - relatively warm air is overtaking it. You also don't get that classic CCB, which really makes for the big events. That's the point of these depictions, in laymen's terms.
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I'm not really feelin' it. At least not yet. The GEFS are strongly pointing to a resurgence to a +NAO regime. The MJO signal to phase 8 is quite strong around that time frame, but does not at all align with the EPS depiction. Therefore I believe the GEFS has a better handle on that timeframe than the EPS currently, and you're going to see the latter trend toward to former, which is more "equal chances" than gang-busters.
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Lol at the 2m temp guidance for this morning. Today is going to be nicest day in a while. Coupled with full march sun. Packs gonna take a beating today. Was too lazy to clean to car off this morning—parked it in the sun towards the front…already doing its work.
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Phase 8 really loses its cold Jan-->Feb--> March. I don't know why. Maybe someone else here can add. Tomorrow being March 1st, and phase 8 happening around mid month, a blend of the two graphics is probably best, but any way, point is: December and January phase 8 ain't nearly the same as March. Seeing some AN tendency sneak into VT, and MA Berks.
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Have to watch this closely - a big drop in the AO, to strongly negative. This isn't a positive for a more snowy outcome, ironically - it will promote the primary phasing with the northern stream, as the PV sags south out of central Canada, and troughing is heavily displaced to the west. More phasing of the primary means more trouble at the mid levels to the north, and less frozen solutions to the south.