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February 2013 mid-long range disco thread


Fozz

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Here's a question before I head off to bed. The NAM is warm with a crappy track, the GFS has a decent track but isn't as wet and still is not cold enough to snow. How do we get the cold air and precipitation? I don't know which set of models is correct. I'll leave that to people either smarter than me or more adventuresome. I will say no matter what the solution, I think snow is getting to be a long shot.

My weenie guess is that the only shot is to get a strong sw to stay a bit more south than the NAM and get a low that bombs on the coast south of us. All of which seems difficult so far.

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My weenie guess is that the only shot is to get a strong sw to stay a bit more south than the NAM and get a low that bombs on the coast south of us. All of which seems difficult so far.

That is the only way, we need dynamic cooling and if the upper low strengthens too soon the primary will still track to far north which will screw us.  Anyway, time for bed. 

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Ha...I gave up on the NAM at 72 hours and then i come back and see it does some funny business after. Encouraging...no, not where we want it, but shows us soclose.

 

It seems there is no model agreement at 500mb.

 

The NAM breaks off vorticity up the Appalachians to PA while the remainder of the system redevelops off NC all

of which gives a weak negative tilt system with a warm nose aloft.  This puts the GFS between the

NAM and the EURO.   I guess folks are staying up for GFS to keep hope alive.

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