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The March 6 Storm- The (last) Great White Hope


stormtracker

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yes...But I am talking about what is probably going to happen :(

 

Yea, i understand. There could be some timing luck in play. Get the first batch of waa late at night and cool the column just right so it would be all snow during the heavier rates during the day....and if the rates stay heavy long enough.....heh...

 

Of course, this was just another dream run before we get punched a couple more times. I think we can safely say this is going to be a big snow event for and area within a 2 hour drive from dca in one direction or another. 

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I don't even know how you can handle all the bashing when few of the weenies who constantly bash it have little clue what these models are doing. That said, the NAM is still a bad numerical model, but I know you have nothing to do with that model.

It's not so bad though some of it is pretty silly.  I try to give information from my/our perspective, and people can decide how to interpret or use that information.  I plead the 5th on the NAM (though you are correct that I have nothing to do with it).

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it can and probably will come further north....and me and you will be dealing with precip type problems...love this rin though....I dont really care if I get a ton of snow...even a few inches would make me happy

 

I'dlike DCA to get enough tmake your winter forecast look good in terms of snow.  I have my doubts that dca would get that much with marginal temps.  On grass I would probably do better than them despite being east but I suspect I'd still get screwed.  I would like someone in the area to get 1958 type snow.  That would be a success. 

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Matt, I'm also thinking the GFS is too warm as is verbatim. Agree about the lower elevations, but this solution would make you beyond happy. Will it happen...well that's another story.

 

But this is probably a best case scenario.  Any more northward shift and we might pay in terms of temps. 

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vinyl, I think you are wrong in saying that phasing brought this storm north, the reason it came north a bit was the block moved out of the way a bit and the ull went positive to negative faster. 

reread my post. I never said this phased. I said it is closer to a phase. Phasing does nothing at this point but help us with cold air, and potentially bomb out the low, but it shouldn't affect VVs, QPF, etc that much.

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Matt, I'm also thinking the GFS is too warm as is verbatim. Agree about the lower elevations, but this solution would make you beyond happy. Will it happen...well that's another story.

Yeah, you really won't get good model output on a computer on this for snowfall when the BL is marginal.  Huge omega and dynamics should give a lot of the borderline areas a paste job.

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So would 00z be the first run with the ULL in the system?  Or will we have to wait till 12z tomorrow?

Looks like the base of the trough should be fully inland by 06z, so 12z for good raob coverage.  Though, I suspect it is close enough to shore (and therefore the airports) that we are getting decent flight-based coverage already.

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I would argue (and would want some of dtk's opinions) that the small details here such as splitting off from the northern stream, some southern stream interaction, and possibly phasing with the northern stream again late is likely adding much more to model difficulties than lack of UA sampling of the upper low. Also, as in most cases, ejecting lows interacting with the complex terrain of the Rockies adds additional variability. It is a tricky UA pattern for the models to handle.

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I would argue (and would want some of dtk's opinions) that the small details here such as splitting off from the northern stream, some southern stream interaction, and possibly phasing with the northern stream again late is likely adding much more to model difficulties than lack of UA sampling of the upper low. Also, as in most cases, ejecting lows interacting with the complex terrain of the Rockies adds additional variability. It is a tricky UA pattern for the models to handle.

 

this and the complex evolution of the pseudo 50/50 feature (which I think honestly has had at least 60 % of the impact)

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new kensington PA and not a met and never seen you post here before,..dont let the door hit your interloping ass on the way out

You make my sides hurt.

 

On a more serious note, is anyone encouraged by the lining up of the GFS, GGEM, NAM, srefs?  I like the agreement.

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I would argue (and would want some of dtk's opinions) that the small details here such as splitting off from the northern stream, some southern stream interaction, and possibly phasing with the northern stream again late is likely adding much more to model difficulties than lack of UA sampling of the upper low. Also, as in most cases, ejecting lows interacting with the complex terrain of the Rockies adds additional variability. It is a tricky UA pattern for the models to handle.

All fair points....it's not like this is a straightforward forecast and a done deal despite the growing consensus.  Just look at how much the solution has evolved over the past 36 hours (despite the similar end result).

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those arent actually snowstorm totals so 1996 is slightly too high and 2003 is slightly too low

It was a bad decision for them to toss aside the snowstorms lists and go to this 1-day, 2-day, 3-day ranking. I know why they did it in terms of climate records, but lumping the clipper snow with the 1/96 blizzard makes no sense. 

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i think it is shortsighted to talk about verification scores and what data is ingested in the model and how by definition it should perform better than 12z in the means since it is 6 hours later....when we all have anecdotal evidence and experience that it is not as skilled in our backyard and often has goofy solutions that are an outlier....In fact there is a certain renowned met who posts in our forum, who has a less than glowing opinion of the off GFS runs, especially 18z, but I will let him speak for himself on that if he wants to

That's fine, but your evidence is purely anecdotal.  In fact, there used to be a considerable gap between 06/18 and the 00/12 cycles, but as the models, assimilation, and observations have improved, this gap has been narrowed consideribly (and in the 4-5 day lead time, basically closed within any statistical significance).  This does not guarantee that this will be the case for any individual discrete, regional event. 

 

I don't really need a lesson on error growth nor data assimilation cycling. 

 

I'd be happy to discuss this in more detail with any renowned met (and if it is who i think you are referring to, will be sure to do so over a beer the next time we are out golfing).

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