Jump to content
  • Member Statistics

    17,601
    Total Members
    7,904
    Most Online
    ArlyDude
    Newest Member
    ArlyDude
    Joined

December 5-6, 2020 Storm Observations and Nowcast


Baroclinic Zone
 Share

Recommended Posts

42 minutes ago, Damage In Tolland said:

Posting on the toll road looks up as he read ends the park ranger 

Definitely not driving as they don’t plow this in winter lol. Buried above 1400- 1500’. Drier top half of accums as you go high. Passed a skier and thanked him for his tracks .

Just Stopped around 1750’ as drifting became an issue even with someone’s boot tracks to use to climb.

Link to comment
Share on other sites

1 hour ago, OceanStWx said:

Trying to dive deep to figure out what the real failure point was here, because I don't really think it was forcing. The QPF was pretty good, right ballpark anyway, clearly there was strong f-gen in the right location relative to the storm. 

I keep coming back to our 00z sounding last night with DGZ up around 500 mb. That's not a great spot and indicative of a pretty torched air mass. Dropping less than dendrite ratios into a deep near freezing layer primed snow to melt at the surface. Even when rates were decent. There was a lot of 1/2 to 3/4SM snowfall that normally would accumulate if your flakes weren't already near slush by the time they reach the ground. Honestly the 04.12z NAM forecast soundings weren't bad in the vicinity of GYX, and it should've been a bigger red flag to me. 

We were running with ratios around 7:1, but they needed to be lower than that given the environment we were working with. Elevations did better because it shrunk the near freezing layer that flakes had to fall through and kept near surface temps slightly cooler. 

I have to go back and find that great paper about dendritic and ice crystal growth but I also remember from it that it talked about how the well-formed dendrites/ice crystals will latently cool more efficiently when they melt than marginal ice crystals. So kind of a double whammy there in a super marginal air mass. 

There was a ton of QPF that fell in the CCB...agreed on that. So it wasn’t like we got dried out over E MA. It just ended up basically being sleet ratios there. 

Link to comment
Share on other sites

2 minutes ago, ORH_wxman said:

I have to go back and find that great paper about dendritic and ice crystal growth but I also remember from it that it talked about how the well-formed dendrites/ice crystals will latently cool more efficiently when they melt than marginal ice crystals. So kind of a double whammy there in a super marginal air mass. 

There was a ton of QPF that fell in the CCB...agreed on that. So it wasn’t like we got dried out over E MA. It just ended up basically being sleet ratios there. 

I wasn't positive of that, but intuitively it makes sense. If you create a crystal at -5C it's going to take less heat to warm it up to 0C than if you create a crystal at -12C. Even if your crystal structure may be more delicate. 

Link to comment
Share on other sites

3 minutes ago, OceanStWx said:

I wasn't positive of that, but intuitively it makes sense. If you create a crystal at -5C it's going to take less heat to warm it up to 0C than if you create a crystal at -12C. Even if your crystal structure may be more delicate. 

Yeah if you’re throwing a bunch of marginal ice crystals at relatively warm temps (like around -5C as you said) into a layer at 32-33F, that sounds uglier than throwing a bunch of hooked dendrites at -10 to -14C into that same layer. 

Link to comment
Share on other sites

10 minutes ago, ORH_wxman said:

I have to go back and find that great paper about dendritic and ice crystal growth but I also remember from it that it talked about how the well-formed dendrites/ice crystals will latently cool more efficiently when they melt than marginal ice crystals. So kind of a double whammy there in a super marginal air mass. 

There was a ton of QPF that fell in the CCB...agreed on that. So it wasn’t like we got dried out over E MA. It just ended up basically being sleet ratios there. 

Is it a mass issue? Melting large aggregated dendrites would remove more heat from the environment than smaller flakes? 

Link to comment
Share on other sites

2 minutes ago, OSUmetstud said:

Is it a mass issue? Melting large aggregated dendrites would remove more heat from the environment than smaller flakes? 

Yeah I’m not sure. The temperature of the ice matters too. I’ll have to search for the paper I mentioned...I think I have it saved on my pc downstairs. It’s like my go-to source for this kind of stuff. It talks about everything including how you can get ice crystals in areas close to the ocean as low as -4C to -5C due to the salt nuclei being far more efficient at warmer temps. 

  • Like 1
Link to comment
Share on other sites

2 minutes ago, ORH_wxman said:

Yeah I’m not sure. The temperature of the ice matters too. I’ll have to search for the paper I mentioned...I think I have it saved on my pc downstairs. It’s like my go-to source for this kind of stuff. It talks about everything including how you can get ice crystals in areas close to the ocean as low as -4C to -5C due to the salt nuclei being far more efficient at warmer temps. 

Right, I usually use -6 out here and then -8 in Ontario, but it's just an estimate because of the stochastic nature of cloud droplets. 

Link to comment
Share on other sites

2 minutes ago, CoastalWx said:

I think spatial area coverage too. Big hooked dendies will be efficient in cooling.

Goes back to what you said originally though Scott how most places didn't see flakes flourish in the DGZ. I remember looking at soundings and x-sections yesterday and saw the same thing. Best lift was either above or below it (at least the stations I was looking at). 

Link to comment
Share on other sites

1 minute ago, OSUmetstud said:

Without the drier dewpoints you also lose any heat of vaporization effects, which is about 8 times larger than the heat of fusion. So you're only left with heat of fusion and a smaller contribution of sensible heat from the flakes themselves. 

Yeah this almost certainly a factor too. Even in warm spring storms, if you have a dry polar high sitting up there, it can be a nice source of drier dewpoints feeding into the storm to help cool the low levels even if temps were 55F the day before. 

There was probably a combo of factors that hurt further east. Less loft in the DGZ, lack of drier dewpoints up north to help advect in a source of lower level cooling. 

  • Like 3
Link to comment
Share on other sites

Just now, It's Always Sunny said:

Goes back to what you said originally though Scott how most places didn't see flakes flourish in the DGZ. I remember looking at soundings and x-sections yesterday and saw the same thing. Best lift was either above or below it (at least the stations I was looking at). 

And the best zone that had decent lift in the DGZ was further west over ORH county into adjacent S NH...so they had the double advantage of better DGZ lift plus some elevation. It’s probably why you saw like 9-12 inches of snow there while Ray in Methuen was struggling to get 2”. You hardly ever see that type of gradient unless he was mostly raining which wasn’t the case. 

  • Thanks 1
Link to comment
Share on other sites

3 hours ago, OceanStWx said:

Well I think a problem is that clown maps (especially these realistic looking ones) are a relatively new feature. Because of how they are generated, you rarely end up seeing more snow than they spit out. 

Point taken.  It still seems like there are more misses these days and model gyrations.  It is not just the maps because you help us see reality.  The Euro no longer dependable, gfs kinda new.  It all just seems less can be counted on from models these days although maybe it is the bias that comes from paying attention more.  It wouldn’t surprise me though that the pace of climate change fooks with the analogue data; Tip has talked about this.  I’m not a scientist so can’t provide any reliable analysis.  But if the Mets don’t feel the models are worse with these storms, then you are probably right since you work with them every day.

Link to comment
Share on other sites

1 minute ago, ORH_wxman said:

And the best zone that had decent lift in the DGZ was further west over ORH county into adjacent S NH...so they had the double advantage of better DGZ lift plus some elevation. It’s probably why you saw like 9-12 inches of snow there while Ray in Methuen was struggling to get 2”. You hardly ever see that type of gradient unless he was mostly raining which wasn’t the case. 

Yeah looking at METARs this morning I was seeing several hours of snow reports for lots of places along the coast but then only saw like 1-2" total.  Unique event for sure and most places changed over sooner than modeled (even though we knew that would probably happen).

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...