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JAN 20th-22nd potential..


NaoPos

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Do you think once tonight/tomorrow system gets out of the way, that will help clarify things or just another day of models getting closer to the "event"

Its more a matter of the shortwaves involved getting on shore. The models will have a better feel for them once they have more physical data as opposed to satellite guesses and a few aircraft readings.

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It sounds like the theme of this winter ;) No resolution until within 48 hours of the prospective event.

In several cases its been a matter of the shortwaves involved getting into the denser RAOB network over land. With dynamic systems like these where they want to blow up right off the coast, the initial conditions are especially critical.

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This looks like a storm where the first event really helps it to possibly track offshore where most people see all snow...this storm has looked like one for several days where if any significant phase occurred it would track just inland of the coast but the first event with the low blowing up to the NE could help the coast's cause.

The one thing to caution is this is sort of a SW flow type system and the NAM has big problems placing these too far south beyond 48 hours.

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In several cases its been a matter of the shortwaves involved getting into the denser RAOB network over land. With dynamic systems like these where they want to blow up right off the coast, the initial conditions are especially critical.

It sounds like a case of a small different in initial conditions resulting in very large differences downstream. Basically, its model roulette until they get properly sampled.

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The differences between the ECM ensemble and the SREF/GFS/CMC is astounding. It is one or the other. Hard to argue against either, but I have to side with the NCEP SREF in the handling of the western wave--but nobody knows for sure. My probabilities will go WAY up if the ECM changes tonite.

Sounds like more sleepless nights ahead :gun_bandana:

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The differences between the ECM ensemble and the SREF/GFS/CMC is astounding. It is one or the other. Hard to argue against either, but I have to side with the NCEP SREF in the handling of the western wave--but nobody knows for sure. My probabilities will go WAY up if the ECM changes tonite.

Understatement. :lol:

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You bring up a pet peeve of mine...

SNOW DOESN'T FREEZE ROCK HARD JUST BECUASE IT IS GONNA GET REALLY COLD.

Sorry for yelling ;)

But seriously, I've heard the media do this time and again... "better shovel the snow before it gets really cold or you'll never get rid of it!" Uh, yeah, how about no! Snow doesn't just magically freeze solid just because it gets really cold after a storm... if it stays all snow (and given the GEM that IS a question right now), then it'll still be snow the next day. It won't magically change into a brick or get heavier or much denser just because the temperature dropped to 5 degrees.

I will rephrase this for you -- that snow which is plowed into your driveway or where salt has mixed in with it. It is only melted snow that freezes like a rock and has melted because of the brine mixture from the roads. Thanks

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The differences between the ECM ensemble and the SREF/GFS/CMC is astounding. It is one or the other. Hard to argue against either, but I have to side with the NCEP SREF in the handling of the western wave--but nobody knows for sure. My probabilities will go WAY up if the ECM changes tonite.

It seems like the Euro and GFS have been duelng this winter. Where one shows a storm several days out and the other doesn't and vice versa. Is it simply due to La Nina or something else?

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This is another improvement. Phase is better and the Dynamic Trop is still coming down.

Out of curiosity, why do you like looking at the 2 PVU surface versus something like DCVA or thermal advection from QG theory? Isn't the 2 PVU surface just indicative of subsidence behind the low (implying that there is more UVV ahead of it)?

This is probably me being a synoptician versus a mesoscale meteorologist.

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It seems like the Euro and GFS have been duelng this winter. Where one shows a storm several days out and the other doesn't and vice versa. Is it simply due to La Nina or something else?

Eh, I don't know if it is La Nina, -NAO, or whatever--they are just different models and work very differently. There will be times they are vastly different.

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Out of curiosity, why do you like looking at the 2 PVU surface versus something like DCVA or thermal advection from QG theory? Isn't the 2 PVU surface just indicative of subsidence behind the low (implying that there is more UVV ahead of it)?

I think IPV thinking is much more succinct at explaining the potential for deep tropospheric cyclogenesis and the development of the cold front through the depth of the atmosphere (and potential folding to enhance rapid/explosive cyclogenesis even more). QG alone doesn't really answer why that 500 hpa vort max "strengthens" as the trough digs from 66-90 hours, and DPVA won't explain it well. IPV thinking also deals nicely with moist processes in the low levels.

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if your in the interior you want and earlier phase. If your in the cities on south and east you do not want an earlier phase.

i think its if your anywhere, you want more digging to get the low to bomb further south. The gfs has been trending this way every single run so far.

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I think IPV thinking is much more succinct at explaining the potential for deep tropospheric cyclogenesis and the development of the cold front through the depth of the atmosphere (and potential folding to enhance rapid/explosive cyclogenesis even more). QG alone doesn't really answer why that 500 hpa vort max "strengthens" as the trough digs from 66-90 hours, and DPVA won't explain it well. IPV thinking also deals nicely with moist processes in the low levels.

Can't it be explained by the strong CAA/WAA couplet, with the very cold air behind the surface low causing heights to crash? Usually, when I think of mid-latitude systems bombing out, it's due to the increasing baroclinicity between the warm and cold sectors. I'm just asking questions, because you are looking at things I don't normally look at when forecasting.

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