Jump to content
  • Member Statistics

    17,598
    Total Members
    7,904
    Most Online
    PublicWorks143
    Newest Member
    PublicWorks143
    Joined

January 6-7 Storm Discussion: we’re due?


WxUSAF
 Share

Recommended Posts

4 minutes ago, usedtobe said:

Personally, in these really marginal temp event,  I use the snow depth product.  It's more conservative with amounts which is a good think. If it's really cold other snow maps are probably preferable.  The GFS snowdepth product from the 18Z run.  

   Good to see you here @usedtobe!      I'm also a huge proponent of the snow depth product in these marginal temperature events, but I like to throw in the caveat that it will be underdone in these type of events if the rates are really good.    

  • Like 6
Link to comment
Share on other sites

8 minutes ago, umdterps29 said:

Is this the type of storm that will have upslope for the Garrett County area? If so, is the upslope intensity usually modeled pretty accurately, or is it typically more/less intense than what is shown on these models?

Garrett County may get some orographic enhancement from the LP as it’s in our area.  Upslope would come on the back-end as the low is heading NE away from the area.  You want to root for the follow up wave that GFS has been keying in to deepen the storm and ‘bomb’ it out for SNE.  That energy as it crosses the mountains and deepens the SLP off the east coast would provide some extra lift for upslope snow showers.  

18z GFS shows this scenario.  Garrett County and the mountains get more snow from the upslope than the initial storm.

  • Like 1
Link to comment
Share on other sites

12 minutes ago, high risk said:

      Do you have an example?    The 10:1 maps should be the same everywhere.     The snow depth maps should be too, except that while Tropical Tidbits only counts positive changes in depth (i.e. they ignore when the amount goes down due to melting or compacting), while others may count any change.      Even the Kuchera method should, in theory, yield the same result across sites.

TT seems to count qpf other sites deem non snow.  It’s always crazy generous on the south side compared to all other outlets. 

  • Like 1
Link to comment
Share on other sites

1 minute ago, psuhoffman said:

TT seems to count qpf other sites deem non snow.  It’s always crazy generous on the south side compared to all other outlets. 

             Assuming you're talking about 10:1 maps?   That's really odd, as the models generate a water equivalent of snow field in mm that should simply be converted to inches and multiplied by 10.      The only thing that they could be doing is trying to make their own determinations about how much of a period of QPF is snow, but that would involve a lot of assumptions on their end that would not work well.     I'd be very interested in seeing an example.

Link to comment
Share on other sites

10 minutes ago, umdterps29 said:

Is this the type of storm that will have upslope for the Garrett County area? If so, is the upslope intensity usually modeled pretty accurately, or is it typically more/less intense than what is shown on these models?

Good upslope requires a stronger surface low than what this storm is offering.

Link to comment
Share on other sites

2 minutes ago, psuhoffman said:

@high risk example 

IMG_0794.thumb.png.f5dd2d3a1350f54aa43c90fae9f8f74d.png
IMG_0793.thumb.png.b3e73c079fb9faa3b50140c702f71fd2.png

       Thanks for this example!    WB must be making their own determinations about how much QPF is going into each precip type.     As I mentioned, the only "accounting" in the actual models (RAP/HRRR excluded) is a snow water equivalent bucket that counts whatever fraction of the falling precip is snow or sleet.     It's "good" in that the WB approach wipes out the sleet and also the accumulations when the profile doesn't support pure snow, but they're trying to match precip the accumulates over a longer period of time with the instantaneous precip type, so that won't always work very well.

       Ultimately, the RAP/HRRR do things the right way:  they have separate buckets for each precip type and output each of them.   It removes the guesswork.    This approach will be used in the new RRFS, and the GFS is going to adopt it too.

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

5 minutes ago, Fozz said:

Good upslope requires a stronger surface low than what this storm is offering.

MLK 2022 was a top 5 favorite storm for me - the upslope was epic for ‘part 2’ of that.  Blizzard conditions at times.  IIRC, you were staying in Accident or close by and chased that event right?  The 500 energy that enhanced the upslope was textbook.  This is definitely not that, ha.

Link to comment
Share on other sites

14 minutes ago, BTRWx's Thanks Giving said:

This particular frame from the euro gives me hope. It tries to stay frozen not far from D.C. almost up to the end of the precip. With these dynamics from this map, would that imply sleet?

euro precip Jan 4_2023 12z.png

Look at my post last page. I used the 3k NAM but I noticed it on the euro. Same thing you’re referencing. 

  • Like 2
Link to comment
Share on other sites

20 minutes ago, usedtobe said:

Personally, in these really marginal temp event,  I use the snow depth product.  It's more conservative with amounts which is a good think. If it's really cold other snow maps are probably preferable.  The GFS snowdepth product from the 18Z run.  s

Snow depth maps are precisely my main influences with my forecast for this system, though with some touch-ups because some web sites will under-do snow depth if the rates can overcome the marginal surface temps.

  • Like 4
Link to comment
Share on other sites

6 minutes ago, high risk said:

       Thanks for this example!    WB must be making their own determinations about how much QPF is going into each precip type.     As I mentioned, the only "accounting" in the actual models (RAP/HRRR excluded) is a snow water equivalent bucket that counts whatever fraction of the falling precip is snow or sleet.     It's "good" in that the WB approach wipes out the sleet and also the accumulations when the profile doesn't support pure snow, but they're trying to match precip the accumulates over a longer period of time with the instantaneous precip type, so that won't always work very well.

       Ultimately, the RAP/HRRR do things the right way:  they have separate buckets for each precip type and output each of them.   It removes the guesswork.    This approach will be used in the new RRFS, and the GFS is going to adopt it too.

Thanks for the info!  

  • Like 1
Link to comment
Share on other sites

6 minutes ago, nj2va said:

MLK 2022 was a top 5 favorite storm for me - the upslope was epic for ‘part 2’ of that.  Blizzard conditions at times.  IIRC, you were staying in Accident or close by and chased that event right?  The 500 energy that enhanced the upslope was textbook.  This is definitely not that, ha.

I was at snowshoe for that. Was epic! 

Link to comment
Share on other sites

6 minutes ago, SnowDreamer said:

@high risk

@Terpeast

The Tropical tidbits map are particularly bad, but they DO say *includes sleet*, so I give them a pass for being way way off. Here's another example from the 3K between WxBell and Pivotal. Granted it's not the most relevant example, but these maps do not look close to me in the circle area. 

Screen Shot 2024-01-04 at 5.10.42 PM.jpg

Screen Shot 2024-01-04 at 5.17.09 PM.png

One is 12z the other 18z

  • Like 2
Link to comment
Share on other sites

8 minutes ago, SnowDreamer said:

@high risk

@Terpeast

The Tropical tidbits map are particularly bad, but they DO say *includes sleet*, so I give them a pass for being way way off. Here's another example from the 3K between WxBell and Pivotal. Granted it's not the most relevant example, but these maps do not look close to me in the circle area. 

Screen Shot 2024-01-04 at 5.10.42 PM.jpg

 

Untitled.jpg

Yes. They are not quite at the point to be correct about micro climates. But they have gotten much better about incorporating elevation into them. Especially the Blue Ridge. Getting better all of the time. 

Link to comment
Share on other sites

2 minutes ago, AtlanticWx said:

this is just a thought but shouldn't the snow stick almost immediately because of how cold the ground is from the two days of pretty cold temperatures along with those 20 degree DPs up until onset? why use snow depth 

Surface temperatures are marginal for a good chunk of the area (just above freezing) and much of the event occurs during daylight hours and questionable snow rates. Getting good rates will be key in the more marginal areas. There's also a relatively stout isothermal layer in the lower levels that will likely hurt accumulation in lighter rates. A lot of the accumulation for the 1-3" crew will depend on how heavy the rates are and how long the heavier rates last.

  • Like 10
Link to comment
Share on other sites

Snow depth is good to check against in marginal situations like this but I’m not sure I’ve ever seen actually accumulations that match snow depth forecasts. Even the December post-deluge changeover beat the snow depths by like a factor of 2.

  • Like 3
Link to comment
Share on other sites

52 minutes ago, EastCoast NPZ said:

T - 2" in the Shen Valley

2 - 4" elevations > 1000 ft.

Areas to the East - good luck.

Mt. PSU could jack in the middle of the Sahara, so 6" for him.

My first and final calls.  Let's see how I do.

4” or bust in your backyard!

I have siblings in Front Royal, Stephens City, Clearbrook and kids in Leesburg and Aldie so I will get their updates.  

I will send you photos next week of the 50 “ plus expected here over the next 8 days

  • Like 2
  • Haha 1
Link to comment
Share on other sites

6 minutes ago, WxUSAF said:

Snow depth is good to check against in marginal situations like this but I’m not sure I’ve ever seen actually accumulations that match snow depth forecasts. Even the December post-deluge changeover beat the snow depths by like a factor of 2.

     That's fair.    The depth field is underdone in events with warm ground going in, marginal temps, and good rates.     But it's a strong alternative to 10:1 maps when you have a lot of sleet (or other mix) or poor rates with marginal temps.     In events that argue for rates overcoming temps, a blend of the 10:1 and snow depth, with a solid lean towards the depth, often works well.  

  • Like 4
Link to comment
Share on other sites

3 minutes ago, clskinsfan said:

I know you have been screwed a lot the past few years. But you are gonna get more than 4 at your new house. I will be completely shocked if I am wrong. These are the storms I promised you that your move would cash in on. 

I'm back in stephens city now.  My old place out in the Junction will probably do ok; I had 1,000' there and it was usually 3F colder than Winchester.  In the low-lands of Stephens City and it's odd UHI, I'm ****ed.  I was here for 10 years prior and I know exactly how these marginal events go.

  • Like 1
  • Haha 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...