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Midwest Thanksgiving Storm...


Powerball

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You mentioned 18 hours in your previous post, not 84.

the vorticity at 18 hours was still much different...I just don't understand how the models work so similar if the higher resolution of the nam causes it to have more vorticity? Doesn't that equal a stronger storm?

I am a layman, so I am just trying to get a better understanding of what i am looking at,.

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NAM has a higher resolution than the GFS.

Quite honestly, the answer is far more complex than what you suggest. Resolution plays little to no role on why, at that particular hour, the NAM has 3-4 units of vorticity (3-4 x 10^-5 /s^1). Also be careful about how it is shaded. Here I could argue they have similar units of vorticity at 84 hours. http://www.twisterdata.com/index.php?prog=forecast&model=NAM&grid=221&model_yyyy=2010&model_mm=11&model_dd=21&model_init_hh=00&fhour=84&parameter=RELV&level=500&unit=MB&maximize=n&mode=singlemap&sounding=n&output=image&view=large&archive=false

http://www.twisterdata.com/index.php?prog=forecast&model=GFS&grid=3&model_yyyy=2010&model_mm=11&model_dd=21&model_init_hh=00&fhour=84&parameter=RELV&level=500&unit=MB&maximize=n&mode=singlemap&sounding=n&output=image&view=large&archive=false

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the vorticity at 18 hours was still much different...I just don't understand how the models work so similar if the higher resolution of the nam causes it to have more vorticity? Doesn't that equal a stronger storm?

I am a layman, so I am just trying to get a better understanding of what i am looking at,.

Well, it is really quite difficult to explain without getting into serious mathematics and dynamics, which includes the primitive equations and/or a lesson in quasigeostrophic theory regarding synoptic meteorology. I talk about some dynamics and quasigeostrophic a bit in this post. Math equations are there but you can understand it if you read it closely. http://jasonahsenmac...nt-1112-142010/

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the vorticity at 18 hours was still much different...I just don't understand how the models work so similar if the higher resolution of the nam causes it to have more vorticity? Doesn't that equal a stronger storm?

I am a layman, so I am just trying to get a better understanding of what i am looking at,.

I don't want to make this too off-topic, but here is another post regarding synoptic meteorology, in this case upper level height falls. Either way, it really is more complex than an issue of resolution. Honestly, if you want to get more in-depth, start a new thread and I will be willing to get more in-depth just so we don't get off-topic here.

http://jasonahsenmacher.wordpress.com/2010/11/10/weak-elevated-convective-instability-associated-with-dynamic-height-falls/

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Quite honestly, the answer is far more complex than what you suggest. Resolution plays little to no role on why, at that particular hour, the NAM has 3-4 units of vorticity (3-4 x 10^-5 /s^1). Also be careful about how it is shaded. Here I could argue they have similar units of vorticity at 84 hours. http://www.twisterda...e&archive=false

http://www.twisterda...e&archive=false

The vorticity that you can see on the NAM is also on the GFS (I agree), but why can you see it more clearly at NCEP on the NAM and not on the GFS?

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Nothing to get excited about at this point, but several of the GFS ensemble members develop a secondary system out of the left over energy in the Southwest.

Interestingly enough the LOLGAPS does too.......Which would make sense with the amount of energy being left over....... Has to be a mirage though...... (maybe reverse psychology will work) :)

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Nothing to get excited about at this point, but several of the GFS ensemble members develop a secondary system out of the left over energy in the Southwest.

Interesting how much variety there was with those ensembles. They are all over the place with this series of systems. Definitely leads one to believe a strong secondary system is still possible. Sort of makes sense given the strong trough and arctic air intrusion. Sometimes when the lead storm ends up riding much further to the north than earlier modeled we end up with a secondary/further south storm. This is obviously a very complex setup, so we definitely don't want to turn our backs to this thing. Not that one person on this board ever would lmao.

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Interesting how much variety there was with those ensembles. They are all over the place with this series of systems. Definitely leads one to believe a strong secondary system is still possible. Sort of makes sense given the strong trough and arctic air intrusion. Sometimes when the lead storm ends up riding much further to the north than earlier modeled we end up with a secondary/further south storm. This is obviously a very complex setup, so we definitely don't want to turn our backs to this thing. Not that one person on this board ever would lmao.

So we would want this to cut as far west and north to give a secondary a chance to pop in time?

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