Jump to content
  • Member Statistics

    17,509
    Total Members
    7,904
    Most Online
    joxey
    Newest Member
    joxey
    Joined

January Medium/Long Range Discussion


WinterWxLuvr
 Share

Recommended Posts

12 minutes ago, mattie g said:

I'll take it, but I'm confused as to how the surface reflects what's going on at 500. Is it because the flow is flatter behind that big storm that in it on the GFS?

This.  I was confused at all the talk of a hit because I was just looking at H5 and never checked surface.   

Link to comment
Share on other sites

20 minutes ago, CAPE said:

No it doesn't matter, but that is just TT p-type suckage.

       To be clear, this isn't a big deal in any way, but it's not a TT issue.     They're using the p-type information directly out of the GFS (and do that for all of the models) and not are computing it on their own.      In lighter precip, the GFS can sometimes overmix the lower levels and warm them up a bit too much, and that appears to be what is happening in that example.

  • Like 1
  • Thanks 4
Link to comment
Share on other sites

21 minutes ago, CAPE said:

No it doesn't matter, but that is just TT p-type suckage.

It is BS but Chuck had one good nugget mixed into his typical word salad this morning which was it’s not that cold given the pattern. The frame he pointed out had a 1040 high in southern Quebec/Ontario with a NW flow and storm off the coast and it was only “average” temps here. I can pick out several days where the “pattern” says it should be a truly bitter cold day but it’s like 40 in DC.  That’s not necessarily 100% relevant to any discreet snow chances since a 40 degree surface temp on a sunny day isn’t relevant to what it would be while precipitating when the dew point is like 12* but it’s still worth mentioning, as @WxUSAF has also noticed, how hard it is to get REALLY cold around here lately. 

  • Like 3
Link to comment
Share on other sites

55 minutes ago, stormtracker said:

Nope.   H5 better, but still flattened/kicked/smooshed/regal beagled

I have never hated an inanimate object more than I hate this ocean low.   I'm legit inconsolable.  

Thank God none of the output today will likely be the final outcome. 

It's way more moving parts than just that ocean storm you hate.  It's also going to depend on spacing with the NS and which STJ waves can time up with one of the NS vorts and how much and when something amplifies.

I can sum up what we're looking at for the next 10 days.  And the good pattern by no means ends there...there are "threats" stacked up in the flow one after another after that on the long range guidance, but I think 10 days out is the furthest we can realistically even guess as the general synoptic setups.  

The rest of this work week were stuck in the NW flow on the backside of the trough and there is no chance for anything of significance.  After that the trough starts to retrograde in response to the north pacific vortex backing off.  The pac jet retraction we have been hearing about.  After that there are 4 NS and 3 STJ SW's in the flow to be watched.  Each likely has more room to amplify than the last.  

The first NS and STJ SW become the ocean hurricane you hate so much and that has virtually no chance to impact our area.  It's coming too soon in the process.  

The second NS vort is the one that could impact our area over the weekend.  It's digging impressively far south for a NS system, it's leaving the next STJ wave behind and going it alone.  The limiting factor with that threat is that it is almost 100% NS and the ocean hurricane you love might be too close limiting its ability to turn the corner and amplify.  It's far enough out though that it has a decent chance and is close enough to something on guidance that I wouldn't be shocked, but suppressed is probably the threat to missing that.

The next threat to watch is around next Tuesday Jan 18th with NS wave 2 and STJ wave 1.  But we have no idea how they interact and if the STJ wave phases or gets left behind again.  All the events before then will impact that threat window.  Still...the general longwave setup heading into that period is even better and this one will have a STJ wave around to be tapped if things come together.  Just at a glance this might be an even better threat than the weekend...with the exception of if the weekend thing blows up it could suppress the next.  There isn't a lot of spacing between these SW's. 

The last threat window I will even speculate on would be later next week around the 20th as another NS SW and STJ wave come east into the trough.  Again...the trough axis and spacing on this one looks good from this range but the details will be determined by what happens with threats 1-2 which are partially impacted by that ocean storm.  

 

There look to be more threats lined up after but now were getting out to total fantasy time ranges.  There is way too much going on in the flow to expect guidance to get any of this right from outside like 4 days or so.  This pattern is absolutely loaded though.  The only way I see a total fail from this would be if the spacing ends up too close between all these waves, and none really amplify and they all split the difference and we get a bunch of weak waves.  But guidance has a hard time resolving exactly what SW to amplify in this type of pattern from range.  I wouldn't worry about that yet.  

  • Like 7
  • Thanks 1
Link to comment
Share on other sites

44 minutes ago, mattie g said:

I'll take it, but I'm confused as to how the surface reflects what's going on at 500. Is it because the flow is flatter behind that big storm that in it on the GFS?

I'm probably way off here but when I was looking at 500, I saw the ocean storm had a different look than GFS and was scooting out of the way - that and the vort diving down from the plains on the CMC was broader in the TN valley than the closed 500 low so I figured it would allow the surface low to reach our area vs being too far SE like the GFS.  It honestly could have been a lucky guess on bad analysis lol

  • Haha 1
Link to comment
Share on other sites

45 minutes ago, high risk said:

       To be clear, this isn't a big deal in any way, but it's not a TT issue.     They're using the p-type information directly out of the GFS (and do that for all of the models) and not are computing it on their own.      In lighter precip, the GFS can sometimes overmix the lower levels and warm them up a bit too much, and that appears to be what is happening in that example.

I only commented because I was looking through the panels on WB for that period and the p-type maps there indicate snow at that same time. I mean temps are 34-35 and the precip at that point is light so it really makes no sensible difference, but I have seen ptype 'disagreements' on TT compared to other sources before, so some interpretation probably with marginal surface temps. Imo people rely too much on those maps instead of looking at the temps through the column and qpf.

  • Like 1
Link to comment
Share on other sites

2 hours ago, stormtracker said:

Just for the record, I'm not debbing at all.  When I deb, that's when you know it's really bad.  I'm just cursing the Gyre from hell on the GFS because it's ****ing everything up on that model. 

We got a good pattern and likely best pattern since the 2013-16 run.  For DC it’s always about the cold source and Mongolia has been sending us some nice nice and Pacific is not belching  Pacific air up into Canada.  

  • Like 1
Link to comment
Share on other sites

4 minutes ago, Cobalt said:

Canadian ensembles agree with the OP. A bit south at the moment, but an impressive precip and snow mean to boot.

cmc-ensemble-all-avg-conus-precip_24hr_inch-2345200.thumb.png.5cbb16c3545a68879b5c518d08d4090d.png

Nice to see the ensembles agree with the OP. If the Euro looks anything like the Canadian, we might be on the way to stealing a third event inside 120 hours this winter.

Link to comment
Share on other sites

59 minutes ago, high risk said:

       To be clear, this isn't a big deal in any way, but it's not a TT issue.     They're using the p-type information directly out of the GFS (and do that for all of the models) and not are computing it on their own.      In lighter precip, the GFS can sometimes overmix the lower levels and warm them up a bit too much, and that appears to be what is happening in that example.

Or no ice nucleation or only very low level lift resulting in drizzle.

Link to comment
Share on other sites

44 minutes ago, NorthArlington101 said:

Webb throwing out the 2018 analog: journey to Charlottesville, anyone?

 

The pacific is a lot more favorable now v that setup but the Atlantic might be even more suppressive. In the end it might end up a wash creating a similar result I’m just pointing out the differences. 

Link to comment
Share on other sites

  • WxUSAF unpinned this topic

Create an account or sign in to comment

You need to be a member in order to leave a comment

Create an account

Sign up for a new account in our community. It's easy!

Register a new account

Sign in

Already have an account? Sign in here.

Sign In Now
 Share

  • Recently Browsing   0 members

    • No registered users viewing this page.
×
×
  • Create New...