AT2k Design BBS Message Area
Casually read the BBS message area using an easy to use interface. Messages are categorized exactly like they are on the BBS. You may post new messages or reply to existing messages!

You are not logged in. Login here for full access privileges.

Previous Message | Next Message | Back to General Weather-related Discussi...  <--  <--- Return to Home Page
   Networked Database  General Weather-related Discussi...   [980 / 2013] RSS
 From   To   Subject   Date/Time 
Message   Mike Powell    All   HVYSNOW: Winter Storm 2/2   February 11, 2025
 9:50 AM *  

FOUS11 KWBC 110852
QPFHSD

Probabilistic Heavy Snow and Icing Discussion
NWS Weather Prediction Center College Park MD
352 AM EST Tue Feb 11 2025

Valid 12Z Tue Feb 11 2025 - 12Z Fri Feb 14 2025


 ... Part 2/2 ....

...Sierra Nevada into much of the West... Days 1-3...

As a large trough amplifies across the Intermountain West, 
upstream shortwaves will begin to dig along the Pacific coast as 
vorticity impulses shed east from an amplifying closed low over the
Pacific. While this low won't really become organized until late 
D3, energy pivoting onshore beginning late D1 will spread an axis 
of moisture into central and southern CA, with snow in the terrain 
above generally 3000-4000 ft. This impulse is weak and will be 
directed almost due SW by the downstream trough, but WPC 
probabilities are moderate (30-50%) for more than 6 inches across 
primarily the southern Sierra D1.5.

After this first impulse, the closed low offshore begins to deepen
and pivot eastward. Height anomalies drop steadily offshore, 
reaching as low as 1st percentile within the CFSR climatology by 
00Z Friday near the CA/OR border, and the accompanying and 
impressive downstream divergence will begin to displace the trough 
with a brief period of shortwave ridging. Increasing moisture 
advection onshore, driven by confluent mid-level flow south of this
closed low topped by a collocated strengthening jet streak will 
surge IVT as high as 500 kg/m/s into the coast late Thursday. This 
will manifest as expanding and intensifying precipitation, with the
accompanying warm front/WAA lifting snow levels rapidly to as much
as 6000 ft in the Sierra. However, farther north into the 
Shasta/Trinity region and into Oregon, pronounced cold air will be 
slow to retreat, leading to some lowland snow potential as well as
overrunning/freezing rain. Moisture will then quickly spread
throughout the Intermountain West through the end of the period
(12z/Fri) along with the progressing, but weakening upper trough.
There continues to be some uncertainty in timing and placement, 
but there is high confidence that this event will eventually result
in heavy wintry precipitation across the West. Current WPC 
probabilities are high (>90%) for 18+ inches across much of the 
Sierra, generally above 4000 ft, and above 70% for 12+ inches (above
3000 ft) in the Shasta/Trinity/Klamath region. This could be quite
impactful to many area passes. Further east into the Intermountain
West and central Rockies, high probabilities (>70%) for at least 8+
inches of snow exists across the Wasatch into the Tushar Mts of
Utah, as well as the San Juan Mts of Colorado.

...Northeast... Days 1 & 3...

Today, a strong cold front will race from the Great Lakes through 
New England, bringing with it an increased risk for convective snow
showers and snow squalls. The high-res CAMs remain aggressive with
their depiction of simulated reflectivity along this front Tuesday
aftn, suggesting a greater threat for snow squalls. The greatest 
risk appears to be from northern Upstate NY across northern New 
England which is where the best overlap of 0-2km fgen and RH 
overlap, and although instability is modest, the SnSq parameter 
does reach +2 across this region on the 00z GFS. This may end up 
more as convective snow showers than true squalls, but briefly 
intense snow rates and restricted visibility could cause dangerous 
travel this afternoon/evening.

Then during the end of D2 and into D3 (centered around 00Z Thursday
to 00z Friday) more widespread significant precipitation will 
overspread the region from SW to NE. This precipitation will be 
associated with a robust low pressure lifting across the Ohio 
Valley, driven by a modest shortwave on the downstream edge of a 
deepening trough over the middle of the CONUS, overlapped with the 
RRQ of a 150 kt poleward arcing jet streak moving across the 
eastern Great Lakes. Downstream of this system, moist advection 
will maximize in response to low- level WAA on S/SE flow 
overrunning a retreating high pressure that will try to wedge back 
to the west into New England. This will result in an expansion of 
wintry precipitation, likely starting as snow everywhere before 
gradually transitioning to sleet and freezing rain, especially 
south of I-90, before winding down Thursday night.

There is growing confidence with the speed of the system, with at 
least moderate snowfall accumulations likely, especially in higher
terrain and northern Maine, as reflected by WPC probabilities that
are above 50% for 4+ inches from the Adirondacks across much of 
northern New England, with >80% probs in northern Maine. 
Additionally, light to moderate icing is possible as reflected by 
WPC probabilities of 10-30% for 0.1" in the Catskills, Berkshires, 
and Litchfield Hills.

Weiss/Fracasso/Snell

...Winter Storm Key Messages are in effect. Please see current 
 Key Messages below...

https://www.wpc.ncep.noaa.gov/key_messages/La...

https://www.wpc.ncep.noaa.gov/key_messages/La...

$$
--- SBBSecho 3.20-Linux
 * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1)
  Show ANSI Codes | Hide BBCodes | Show Color Codes | Hide Encoding | Hide HTML Tags | Show Routing
Previous Message | Next Message | Back to General Weather-related Discussi...  <--  <--- Return to Home Page

VADV-PHP
Execution Time: 0.0201 seconds

If you experience any problems with this website or need help, contact the webmaster.
VADV-PHP Copyright © 2002-2025 Steve Winn, Aspect Technologies. All Rights Reserved.
Virtual Advanced Copyright © 1995-1997 Roland De Graaf.
v2.1.250224