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February 16-17, 2024 | NE / Mid-Atlantic Winter Storm


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Found this on another forum……

 

Thundersnow incoming?

From 1023 AFDLWX:
Some lightning was being
detected over southern Missouri, indicating elevated instability
and strong, deep lift via low-level frontogenesis and very
strong upper-level divergence in the left exit region of an
incoming jet streak.
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5 minutes ago, Wtkidz said:

Found this on another forum……

 

Thundersnow incoming?

From 1023 AFDLWX:
Some lightning was being
detected over southern Missouri, indicating elevated instability
and strong, deep lift via low-level frontogenesis and very
strong upper-level divergence in the left exit region of an
incoming jet streak.

Yes, I posted the SPC Convection Outlook D1, a few pages back. I was making that point about it bringing more "juice" due to the convective nature of the incoming parcels. 

image.thumb.png.f9ff76ede5dfb294d38194f9326da6ec.png

Edited by Undertakerson2.0
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We got about 3 inches overnight, sometime the snow was intense (I was driving in it at one point and it was snow tunnel driving).  But I think that's all we get from this system.   Main portion going much farther south.

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8 minutes ago, Wtkidz said:

Swear the storms gonna just go north of me… well it has to start and end somewhere. 

Wtkidz, it looks like you are in line for a couple of inches, correct? Really hoping for your sake you get some. 

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6 minutes ago, Gardyloo said:

We got about 3 inches overnight, sometime the snow was intense (I was driving in it at one point and it was snow tunnel driving).  But I think that's all we get from this system.   Main portion going much farther south.

I'm Confused

You speaking of two different systems - the clipper from last night and then mentioning this one? 

Or are you only speaking about last night? 

Or are you saying you think last night and tonight are the same? 

Your location suggests you got last night's clipper - (light snow even as far S as Clapper and Me in C PA) and that you're "farther south" reference is to this one tonight. Is that correct? 

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16 minutes ago, Undertakerson2.0 said:

I'm Confused

You speaking of two different systems - the clipper from last night and then mentioning this one? 

Or are you only speaking about last night? 

Or are you saying you think last night and tonight are the same? 

Your location suggests you got last night's clipper - (light snow even as far S as Clapper and Me in C PA) and that you're "farther south" reference is to this one tonight. Is that correct? 

I got the clipper, so yes, I am speaking of the other one, my apologies.  We also got a nice band of lake effect.  Just to confuse things more.  (should of been in the clipper thread which I hadn't noticed)

 

Edited by Gardyloo
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20 minutes ago, CandO100 said:

Wtkidz, it looks like you are in line for a couple of inches, correct? Really hoping for your sake you get some. 

Thanks  I am very used as the rain snow line  seems to run right through our area even with a Miller system. Unless we have perfect track we tend to have mixing issues. It will depend on thermals.
 

I just enjoy tracking weather  . This  one has been fun for me as it wasn’t as hectic as many storms in the past. 

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49 minutes ago, Wtkidz said:

IMG_0644.jpeg

As an admitted snow weenie, my definition of "worst case" is significantly different than the NWS.

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1 hour ago, Paletitsnow63 said:

12Z GGEM not as robust with snow as other 12Z models but an increase over 0Z

 

trend-gdps-2024021612-f036.sn10_acc-imp.us_maCCCMMM.gif

Some of that has to do with ratios, that’s 10:1 while the others are kuchera, northern ratios are higher. 
 

edit: I noticed some of your maps from last page are 10:1 as well, my mistake. 

Edited by TLChip
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2 hours ago, Undertakerson2.0 said:

They callin this a clipper but it's not really. It's more of a hybrid between a clipper and a standard over-running event. Clips don't often get ANY help from the S jet and this, as we've shown, gets a piece of the STJ moisture.

Asking just so I’m not mixing them up

Clipper = norther stream energy typically moving towards the south-east. Typically under 4” accumulation in large area, can cause squalls/whiteouts. 

overruning = fropa type setups(??), warm in front cold behind, typically pulling up moisture from the south. Can surprise and drop very solid snowfalls, tend to be smaller areas of high snowfall. Lots of mixing areas. 

Phased = interaction between both jets with a closed low. What most of us live here for. 

Edited by TLChip
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3 minutes ago, TLChip said:

Asking just so I’m not mixing them up

Clipper = norther stream energy typically moving towards the south-east. Typically under 4” accumulation in large area, can cause squalls/whiteouts. 

overruning = fropa type setups(??), warm in front cold behind, typically pulling up moisture from the south. Can surprise and drop very solid snowfalls, tend to be smaller areas of high snowfall. Lots of mixing areas. 

Phased = interaction between both jets with a closed low. What most of us live here for. 

Hence my using "hybrid" to define it. 

This starts in the N PAC and comes in via the WA and BC border. From there it went down to SE CO as we discussed last night. Now is in TX where it is gaining some convective juiciness. So that part of "typically moving towards SE" is solid. HOWEVER, it then come NE towards us - from a trajectory that is mostly seen in over-running events or what we sometimes call a SWFE (southwest flow event) So that part of the track is Over Runner type (it doesn't dig so we can't say its a long wave either).

This is no phasing situation, so redevelopment noted at Delmarva is not a phase - it is a slight pause while the layers stack. The layers stacking leads to enhanced impact. 

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Wow an novella from Sterling.

 

NEAR TERM /THROUGH SATURDAY/...
As of mid morning, a pair of mid/upper-level shortwaves were
digging across the Upper Midwest toward the Ohio River Valley.
At the surface, a front was stalled near the North/South
Carolina border, extending west to central Arkansas where a
surface low was developing. IR satellite had what loosely
resembled a baroclinic leaf developing over the lower Ohio River
Valley north of the surface low. Some lightning was being
detected over southern Missouri, indicating elevated instability
and strong, deep lift via low-level frontogenesis and very
strong upper-level divergence in the left exit region of an
incoming jet streak.

Trends will be closely monitored through the day upstream, as
this system will be moving quickly eastward through tonight,
bringing snow to the Mid-Atlantic.

Clouds will increase through the day as the system approaches
from the west. The daylight hours are expected to be dry, with
snow reaching the Appalachian crest early this evening. The snow
will spread rapidly eastward through the evening hours, becoming
heavy at times due to the strong forcing.

Aloft, there will be strong PVA as well as upper-level
divergence via the left exit region of a 180-200 knot jet. In
the low/mid-levels, intense WAA and isentropic lift/fgen is
anticipated north of the surface low. This intense, deep lift
stretches through the DGZ which will be deepening especially
north of US-50/I-66 tonight. For this reason, believe snowfall
rates may reach 1-2 inches per hour as heavier bands develop.
Although the steadiest snow will likely only last 3-4 hours in
any one spot, areas that are under heavier bands for most of
this time could see 5-8 inches given the higher rates, and that
is reflected in the high end (90th percentile) graphics. Areas
with stronger orographic lift (the northern Virginia Blue Ridge
and the Allegheny/Potomac Highlands and Catoctins) could even
see a little more enhancement on top of that.

The areas that are most likely to see warning-level accumulation
appear to be our climo-favored areas north and west of the urban
corridor. This is where the DGZ looks deeper and the surface
temperatures will be a few degrees colder, reducing or
eliminating any brief initial melting of snow. This area is also
favorably placed 100-150 miles north/west of the surface low
track and just north of the H85 low track, with a favorable
overlap of upper divergence/low-level fgen. It should be noted
that some guidance and upstream trends show the potential for
multiple bands of heavy snow, one perhaps more jet induced by
upper-level forcing (higher ratios/deeper DGZ, but less QPF),
with another driven more by low-level fgen (somewhat lower
ratios but higher QPF). Between these bands, there may be a bit
of subsidence and relative minima in QPF/snow. Confidence is a
bit lower, especially further east where surface temperatures
will be a touch warmer to start.

This is a rapidly-evolving situation, so it`s important to check
back through the day for updates.

Precipitation should exit the region as the low moves offshore
by daybreak Saturday, except perhaps (1) right near the
Chesapeake Bay closer to the departing low, (2) across northern
Maryland where lingering lift via the mid/upper wave could cause
some snow to linger, and (3) along/west of the Allegheny Front
where some residual upslope is possible.

During the day Saturday looks mostly dry, though stratocu likely
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Mesoscale Discussion 0145
   NWS Storm Prediction Center Norman OK
   1126 AM CST Fri Feb 16 2024

   Areas affected...portions of eastern Illinois into central Indiana
   and western Ohio

   Concerning...Heavy snow 

   Valid 161726Z - 162130Z

   SUMMARY...Occasional bouts of heavy snow are possible through early
   afternoon, with up to 1 inch/hr snowfall rates and reduced
   visibility possible.

   DISCUSSION...A 500 mb jet streak continues to overspread the OH
   Valley, which is encouraging 850-700 mb warm-air and moisture
   advection
. The low-level warm-air advection trends are increasing
   the magnitudes of 700 mb frontogenesis, with deep-layer ascent
   strengthening within deepening/moistening dendritic growth zone.
At
   least a few reports of heavy snow have been received within the past
   few hours and this trend is expected to continue through the
   afternoon. Up to 1 inch/hr snowfall rates will remain possible,
   along with brief periods of reduced visibility associated with an
   east-to-west oriented snowband.

image.thumb.png.ab6756833616d596ff5d9a66c9c1ae4c.png

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