Jump to content
  • Member Statistics

    17,611
    Total Members
    7,904
    Most Online
    NH8550
    Newest Member
    NH8550
    Joined

January 17-18 Winter Storm


Snowstorms
 Share

Recommended Posts

51 minutes ago, IWXwx said:

The 06z GFS was showing something similar, but I don't have a clue.

EDIT: My bad, that's the 12z

Screenshot_2020-01-14 Models GFS — Pivotal Weather.png

I believe it is due to the abnormally dry air off to the east of the low. Typically the cold conveyor belt moistens as it flows under the warm conveyor belt when wrapping around a storm and dries off a bit turning into snow on the backend of a low. This is honestly a perfect CAD example as you can see how as this moves east it drops freezing rain/sleet all over the Apps

Link to comment
Share on other sites

5 hours ago, Snowstorms said:

2011-12, 2012-13 and 2015-16 were worse up until now. 

 

2011-12 was a lovely winter in my opinion. It does stink when the snowmobile and ice skates stay in the garage but the weather was beautiful and sunny which was a nice reprieve considering what was on the horizon.

I think 2013-14 was honestly overwhelming, the constant snow and cold just wore you down.  I do like snow, but 86" was too much for me

  • Like 2
Link to comment
Share on other sites

DVN has 100% snow in the point for here.  Interesting.

 

Friday  Snow, mainly after 7am. High near 32. Chance of precipitation is 90%. New snow accumulation of 1 to 2 inches possible.
Friday Night  Snow. Low around 28. Chance of precipitation is 90%.
Saturday  Snow, mainly before 1pm. High near 34. Breezy. Chance of precipitation is 90%.

 
 
 
 
 
Link to comment
Share on other sites

DVN has 100% snow in the point for here.  Interesting.   Friday  Snow, mainly after 7am. High near 32. Chance of precipitation is 90%. New snow accumulation of 1 to 2 inches possible. Friday Night  Snow. Low around 28. Chance of precipitation is 90%.

Saturday  Snow, mainly before 1pm. High near 34. Breezy. Chance of precipitation is 90%.

         

 

 

The reason for that is they still use the first generation top down methodology for p-type derivation, max wet bulb temp aloft. It's fine as a proxy but the modified Bourgoin wet bulb energy method provides better results with less potent warm noses but enough positive energy for full melting and not enough low level negative energy for refreezing. In max Tw aloft, probabilities are set to certain temp thresholds, so anything below 2C aloft has increasingly high snow probs and less sleet, 2-3C has max sleet probs and above 3C has highest ZR probs.  

The work done by my co-workers, who are getting a paper published on modified Bourgoin, has real sounding cases that show the max Tw aloft method causes too much sleet and snow and not enough ZR in a lot of cases. On the other hand, when a fairly potent warm nose is undercut by a pronounced low level cold wedge, that method won't produce enough sleet.  

 

The energy method is the way the agency is going and it's what's being used for experimental probability of weather type grids in the NBM, but they still haven't brought all offices on the same page. So for offices west of GRB, MKX, LOT, ILX, they're still using max wet bulb temp aloft, creating an unfortunate discrepancy. Once confidence increases in the scenario closer in, I'm sure they'll do more to have better interoffice consistency with the weather grids.

 

 

 

 

 

 

 

 

 

  • Like 5
  • Thanks 3
Link to comment
Share on other sites

53 minutes ago, RCNYILWX said:

The reason for that is they still use the first generation top down methodology for p-type derivation, max wet bulb temp aloft. It's fine as a proxy but the modified Bourgoin wet bulb energy method provides better results with less potent warm noses but enough positive energy for full melting and not enough low level negative energy for refreezing. In max Tw aloft, probabilities are set to certain temp thresholds, so anything below 2C aloft has increasingly high snow probs and less sleet, 2-3C has max sleet probs and above 3C has highest ZR probs.  

The work done by my co-workers, who are getting a paper published on modified Bourgoin, has real sounding cases that show the max Tw aloft method causes too much sleet and snow and not enough ZR in a lot of cases. On the other hand, when a fairly potent warm nose is undercut by a pronounced low level cold wedge, that method won't produce enough sleet.  

 

The energy method is the way the agency is going and it's what's being used for experimental probability of weather type grids in the NBM, but they still haven't brought all offices on the same page. So for offices west of GRB, MKX, LOT, ILX, they're still using max wet bulb temp aloft, creating an unfortunate discrepancy. Once confidence increases in the scenario closer in, I'm sure they'll do more to have better interoffice consistency with the weather grids.

 

 

 

 

 

 

 

 

 

The energy methods that you talk about are enlightening... sort of treating it as an integrated value like CAPE is.  I have a question though.  I have no idea where I got this from but a long time ago I read that in situations with a warm layer aloft, having -4C or colder in the cold layer greatly increases the chance for sleet, even if the warm layer aloft is pretty warm.  How well do you think that works? 

  • Like 1
Link to comment
Share on other sites

The energy methods that you talk about are enlightening... sort of treating it as an integrated value like CAPE is.  I have a question though.  I have no idea where I got this from but a long time ago I read that in situations with a warm layer aloft, having -4C or colder in the cold layer greatly increases the chance for sleet, even if the warm layer aloft is pretty warm.  How well do you think that works? 

The energy method works on that basis because it is so intuitive and mirrors severe weather forecasting. An integrated value tells you a lot more than a point value, like CAPE and CIN and iterations of both, versus LI, K Index and totals totals. Not that there's no use for more simplistic measurements, but they oversimplify the atmosphere.

-4 to -5 C is definitely a decent rule of thumb or proxy and one I've used before. You'd figure to have that magnitude of cold underlying a warm layer, it would have a decent amount of negative energy.

Sent from my SM-G965U using Tapatalk

Link to comment
Share on other sites

00z NAM was still fairly bullish on ice.  Certainly some negative factors for getting really big ice amounts in this setup, like duration (maybe only about 3-6 hours tops in a given location) and surface WAA.  But it could still get a little dicey, and it doesn't take much to start causing problems with trees/powerlines when you add some wind, and it should be at least a little breezy with a decent pressure gradient.  

Link to comment
Share on other sites

18 minutes ago, Hoosier said:

00z NAM was still fairly bullish on ice.  Certainly some negative factors for getting really big ice amounts in this setup, like duration (maybe only about 3-6 hours tops in a given location) and surface WAA.  But it could still get a little dicey, and it doesn't take much to start causing problems with trees/powerlines when you add some wind, and it should be at least a little breezy with a decent pressure gradient.  

Even tho the window may be a short one, I'm seeing a much greater risk of icy roadways with the much colder sub-freezing temps leading into the event. Unlike the last 2, when it was 50s in the morning before dropping to freezing afterwards. Ofc, that's tricky as well, since the main roads should be getting scraped & treated (with temps rising chem's will be much more effective) thus you'd lean towards secondary roads being more likely to ice up, but they are less likely to be scraped and if snow-covered, it will mitigate any ZR. As you say tho, there's the off surface concerns too. 

Link to comment
Share on other sites

14 minutes ago, StormChaser4Life said:

This storm is certainly not trending in a good way. At least for me. Slower timing which allows temperatures to moderate quite a bit giving a much shorter window of wintry precipitation 

Yeah. 0z NAM has SLP way north, tho still keeps me mostly snow/frozen. Not a fan of that look, but WPC actually put most of the Mitt in the Hvy Snow contour with today's release. I'm cautiously hopeful for a 4-ish thump of wetter snow, a period of mix, maybe a not too long window of liquid, followed by a change to backside snow and LEhs>>LES on Sunday (have Snow Likely in my grid for Sunday actually). 

  • Like 1
Link to comment
Share on other sites

Interesting stat: Toledo OH gets exactly 5.2" (Kuchera ratios) with the 00z GFS and 00z Canadian. With this storm, the borderline of rain/snow is going to be hard to forecast, and may come down to nowcasting, so this consistency means almost nothing at this point.

  • Thanks 1
Link to comment
Share on other sites

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...