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3/23 - 3/24 Winter Storm


NEG NAO

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It's a bit light on the qpf.. Maybe 1/2 to 3/4 inch, but I guess this model has been consistently the driest anyhow

yeah thats not too bad, it looked like less when i was looking at the 6hr frames. Either way, the low is still way south of the gfs and colder. GFS is an outlier

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Fascinating talking about snow here while SPC D2 discussion has them talking about a possible moderate risk for the Ohio Valley.

Yeah, this is a crazy synoptic setup

day2probotlk_0600_any.gif

...OHIO/TENNESSEE VALLEYS INTO THE MID ATLANTIC COAST...

INITIAL STORM DEVELOPMENT MAY BE FOCUSED IN THE WARM SECTOR NEAR THE

LOW...AND ALONG THE FRONTAL ZONE TO THE EAST SOUTHEAST OF THE

LOW...PERHAPS AS EARLY AS MID DAY ACROSS PARTS OF SOUTHEASTERN

INDIANA INTO OHIO. THIS MAY INCLUDE SUPERCELLS...BUT UPSCALE GROWTH

INTO AN EVOLVING MESOSCALE CONVECTIVE SYSTEM APPEARS

POSSIBLE...WHICH SHOULD DEVELOP SOUTHEASTWARD THROUGH THE CENTRAL

APPALACHIANS BY LATE AFTERNOON.

AS THIS OCCURS...AND AN AREA OF STRONG MID/UPPER FORCING FOR UPWARD

VERTICAL MOTION BEGINS TO OVERSPREAD THE REGION WITH THE APPROACHING

UPPER JET STREAK...ADDITIONAL STORM DEVELOPMENT IS EXPECTED

SOUTHWESTWARD ALONG AN EFFECTIVE DRY LINE TYPE STRUCTURE NEAR AND TO

THE SOUTHEAST OF THE OHIO RIVER. THIS ACTIVITY MAY TEND TO REMAIN

DISCRETE IN THE PRESENCE OF FAVORABLE SHEAR FOR SUPERCELLS.

TORNADIC POTENTIAL...PARTICULARLY WITH THE DISCRETE STORMS...

REMAINS THE PRIMARY UNCERTAINTY FOR THIS FORECAST...AND APPEARS

LIKELY TO HINGE ON THE CHARACTER OF THE BOUNDARY LAYER. WHILE

LOW-LEVEL HODOGRAPHS IN GENERAL MAY NOT BECOME PARTICULARLY LARGE

AND CLOCKWISE CURVED...THE SHEAR STILL APPEARS SUFFICIENT.

HOWEVER...FORECAST SOUNDINGS AMONG THE MODELS DO EXHIBIT SOME

VARIABILITY CONCERNING THE BOUNDARY LAYER MOISTURE CONTENT. IF

SURFACE DEW POINTS APPROACH 60F...AND THE SURFACE DOES NOT HEAT TOO

STRONGLY AND SUPPORT DEEPER MIXING...THE TORNADO POTENTIAL MAY BE

HIGHER...AND THE SEVERE THREAT PERHAPS GREATER THAN REFLECTED BY THE

CURRENT SLIGHT RISK. CURRENTLY...IT SEEMS MORE PROBABLE THAT

SLIGHTLY DRIER BOUNDARY LAYER CONDITIONS WILL PREVAIL...PROMOTING

PRIMARILY A LARGE HAIL AND DAMAGING WIND THREAT.

MODEST DESTABILIZATION AND INCREASING LARGE-SCALE ASCENT COULD ALSO

PROMOTE STRONG/SEVERE STORM DEVELOPMENT TO THE LEE OF THE CENTRAL

APPALACHIANS BY LATE AFTERNOON. BUT IT ALSO SEEMS POSSIBLE THAT THE

MESOSCALE CONVECTIVE SYSTEM MAY MAINTAIN STRENGTH ACROSS THE

APPALACHIANS...WITH A CONTINUING SEVERE THREAT ACROSS PARTS OF

VIRGINIA AND NORTH CAROLINA DURING THE EVENING HOURS. COOL/COLD AIR

TO THE NORTH OF A STALLED FRONTAL ZONE MAY MITIGATE THE SEVERE STORM

POTENTIAL NEAR CHESAPEAKE BAY AND ACROSS NORTHERN VIRGINIA.

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Yeah, this is a crazy synoptic setup

day2probotlk_0600_any.gif

...OHIO/TENNESSEE VALLEYS INTO THE MID ATLANTIC COAST...

INITIAL STORM DEVELOPMENT MAY BE FOCUSED IN THE WARM SECTOR NEAR THE

LOW...AND ALONG THE FRONTAL ZONE TO THE EAST SOUTHEAST OF THE

LOW...PERHAPS AS EARLY AS MID DAY ACROSS PARTS OF SOUTHEASTERN

INDIANA INTO OHIO. THIS MAY INCLUDE SUPERCELLS...BUT UPSCALE GROWTH

INTO AN EVOLVING MESOSCALE CONVECTIVE SYSTEM APPEARS

POSSIBLE...WHICH SHOULD DEVELOP SOUTHEASTWARD THROUGH THE CENTRAL

APPALACHIANS BY LATE AFTERNOON.

AS THIS OCCURS...AND AN AREA OF STRONG MID/UPPER FORCING FOR UPWARD

VERTICAL MOTION BEGINS TO OVERSPREAD THE REGION WITH THE APPROACHING

UPPER JET STREAK...ADDITIONAL STORM DEVELOPMENT IS EXPECTED

SOUTHWESTWARD ALONG AN EFFECTIVE DRY LINE TYPE STRUCTURE NEAR AND TO

THE SOUTHEAST OF THE OHIO RIVER. THIS ACTIVITY MAY TEND TO REMAIN

DISCRETE IN THE PRESENCE OF FAVORABLE SHEAR FOR SUPERCELLS.

TORNADIC POTENTIAL...PARTICULARLY WITH THE DISCRETE STORMS...

REMAINS THE PRIMARY UNCERTAINTY FOR THIS FORECAST...AND APPEARS

LIKELY TO HINGE ON THE CHARACTER OF THE BOUNDARY LAYER. WHILE

LOW-LEVEL HODOGRAPHS IN GENERAL MAY NOT BECOME PARTICULARLY LARGE

AND CLOCKWISE CURVED...THE SHEAR STILL APPEARS SUFFICIENT.

HOWEVER...FORECAST SOUNDINGS AMONG THE MODELS DO EXHIBIT SOME

VARIABILITY CONCERNING THE BOUNDARY LAYER MOISTURE CONTENT. IF

SURFACE DEW POINTS APPROACH 60F...AND THE SURFACE DOES NOT HEAT TOO

STRONGLY AND SUPPORT DEEPER MIXING...THE TORNADO POTENTIAL MAY BE

HIGHER...AND THE SEVERE THREAT PERHAPS GREATER THAN REFLECTED BY THE

CURRENT SLIGHT RISK. CURRENTLY...IT SEEMS MORE PROBABLE THAT

SLIGHTLY DRIER BOUNDARY LAYER CONDITIONS WILL PREVAIL...PROMOTING

PRIMARILY A LARGE HAIL AND DAMAGING WIND THREAT.

MODEST DESTABILIZATION AND INCREASING LARGE-SCALE ASCENT COULD ALSO

PROMOTE STRONG/SEVERE STORM DEVELOPMENT TO THE LEE OF THE CENTRAL

APPALACHIANS BY LATE AFTERNOON. BUT IT ALSO SEEMS POSSIBLE THAT THE

MESOSCALE CONVECTIVE SYSTEM MAY MAINTAIN STRENGTH ACROSS THE

APPALACHIANS...WITH A CONTINUING SEVERE THREAT ACROSS PARTS OF

VIRGINIA AND NORTH CAROLINA DURING THE EVENING HOURS. COOL/COLD AIR

TO THE NORTH OF A STALLED FRONTAL ZONE MAY MITIGATE THE SEVERE STORM

POTENTIAL NEAR CHESAPEAKE BAY AND ACROSS NORTHERN VIRGINIA.

I really hate this setup because it is not fair the Ohio valley gets the severe weather and NYC gets a possible all snow event? How could this ever happen? Chicago was getting severe weather too? I hate this weather pattern? This is the season for thunderstorms to come not snow? Death to the computer model.

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I really hate this setup because it is not fair the Ohio valley gets the severe weather and NYC gets a possible all snow event? How could this ever happen? Chicago was getting severe weather too? I hate this weather pattern? This is the season for thunderstorms to come not snow? Death to the computer model.

It isn't really t-storm season around here yet. Our t-storm season doesn't really get going until later in Spring when it warms up more.

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It isn't really t-storm season around here yet. Our t-storm season doesn't really get going until later in Spring when it warms up more.

At least I don't want a snowstorm out of this or I begging not all snow. This is the late March. I want snow is when it is winter. After 75 degree and I am in the spring. This setup is just weird because places to northwest gets rain or mixed precip and NYC gets all snow why is this?

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At least I don't want a snowstorm out of this or I begging not all snow. This is the late March. I want snow is when it is winter. After 75 degree and I am in the spring. This setup is just weird because places to northwest gets rain or mixed precip and NYC gets all snow why is this?

Confluence, confluence, confluence.

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For my money, I'm taking the colder WRF for this storm. I have seen this before where the GFS was way north with the milder 850 temps, only to cave to the consistently colder WRF in the end. It happened earlier this season with a wave just like this one coming W to E and I think it's going to happen again.

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.SHORT TERM /TONIGHT THROUGH THURSDAY/...

SHARP FRONTAL BOUNDARY EXTENDS ATTM ACROSS THE CENTRAL PLAINS INTO

THE OH VALLEY...AND SHOULD APPROACH AS A WARM FRONT LATE TONIGHT

INTO WED AS LOW PRESSURE IN THE LEE OF THE ROCKIES MOVES TO THE OH

VALLEY. PREFER A MORE SUPPRESSED NAM/ECMWF BLEND FOR EVOLUTION OF

THIS SYSTEM...WITH SFC HIGH PRESSURE HOLDING ON LONGER THAN IN THE

GFS...AND WITH A MORE REALISTIC SECONDARY DEVELOPMENT OFF THE

DELMARVA COAST AS THE PRIMARY LOW APPROACHES THE APPALACHIANS.

THE GFS BY COMPARISON APPEARS TO BE ERODING THE HIGH TOO

QUICKLY...WITH TOO CONSOLIDATED A LOW CROSSING THE APPALACHIANS

AND NO SECONDARY DEVELOPMENT...WHICH IN TURN ALLOWS TOO MUCH WARM

AIR TO INTRUDE ALOFT.

TEMPS ALOFT WILL BE COLD ENOUGH FOR SNOW...SO BOUNDARY LAYER

TEMPS SHOULD ULTIMATELY DRIVE PRECIP TYPE...SNOW IN MOST PLACES

EXCEPT FOR NYC METRO...WHERE A SNOW/RAIN MIX IS MORE

LIKELY...PERHAPS A PERIOD OF ACCUMULATING SNOW MAINLY IN THE

MORNING BEFORE E-SE FLOW BRINGS IN SLIGHTLY WARMER AIR.

FCST MODELS INDICATE POTENTIAL FOR A BAND OF ENHANCED LIFT VIA

H7-8 FRONTOGENESIS THAT SHOULD MOVE SW-NE ACROSS THE AREA FROM

LATE MORNING INTO THE AFTERNOON...THAT WOULD BRING AT LEAST

ADVISORY CRITERIA SNOWFALL OF 2-4 OR 3-5 INCHES TO INTERIOR

PORTIONS OF NE NJ...THE LOWER HUDSON VALLEY AND SW CT. OF THESE

AREAS...ORANGE AND WESTERN PASSAIC COUNTIES STAND A CHANCE OF

SEEING AMOUNTS OF OVER 6 INCHES...BUT WITH ECMWF AND NAM IN

CONFLICT ON QPF...THE LATTER A LITTLE MORE SUPPRESSED AND

DRIER...TO SAY NOTHING OF INHERENT UNCERTAINTIES IN PREDICTING THE

EXACT LOCATION AND INTENSITY OF MESOSCALE BANDING MORE THAN 24 HR

IN ADVANCE...DID NOT HAVE A HIGH ENOUGH CONFIDENCE LEVEL TO ISSUE

A WINTER STORM WATCH.

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I strongly feel that NYC and LI will see a slushy 1-2 accum during the day on 3/23 and gets 4-6 inches additional from 3/23 6PM evening through 3/24 3AM. The evening period looks like heavy snow with deform banding and comma head developing over the region. Definitely a plowable snow for NYC and LI per the NAM and ARW which are the high res models. Weekend event looks suppressed and not a big deal. It looks like the next week event is either HECS or nothing depending on the situation as it gets closer. That probably is the last chance and maybe the chance for a foot of snow. Next week is the closest we'll ever get in many decades to 4/1982 pattern for a spring blizzard. The upcoming pattern reminds me of the 12/19 to 12/28 pattern ....... Once past 4/5 it looks like the pattern will have no choice but to relax significantly or very slowly collapse. It looks like the first week of April is a wasting Arctic airmass over the northeast that is forced to modify greatly. After that first week, April will likely have a torch or warmer period. This will be our rapid leaf out period from 4/10 to 4/25. We will get there and rather pay with cold for the next two weeks than have this happen from 4/10 to 4/25.

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NYC and coast will be fighting boundary temps.

Only way NYC gets good snow is for precip to be heavy and especially at night.

Euro has heaviest precip falling tomorrow daytime and took away the heavier precip tomorrow night.

For the coast to get more then 2"-3", we must get that heavy burst of precip that some models are hinting at tomorrow night. Without it, I can't see coast getting more then 1"-2" of slush total.

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There will likely be two periods of significant precip.

First, a 3-6 hour period of light-moderate overrunning precip. mid-late Wed morning into early afternoon.

Second, a ~9 hour period of moderate to heavy precip. associated with the developing coastal low from around 8PM to 4AM Wed night. For NYC and LI, this second period should comprise the bulk of the precip (at least two-thirds).

3Z ETA and many of the ETA-based SREF members have the best handle on the upper-level features and these 2 separate periods of precip, IMHO.

NYC and coast will be fighting boundary temps.

Only way NYC gets good snow is for precip to be heavy and especially at night.

Euro has heaviest precip falling tomorrow daytime and took away the heavier precip tomorrow night.

For the coast to get more then 2"-3", we must get that heavy burst of precip that some models are hinting at tomorrow night. Without it, I can't see coast getting more then 1"-2" of slush total.

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