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March 23 Severe disc/obs


Ellinwood

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Full discussion coming later today. For now, SPC:

day2probotlk_20110322_0600_any_prt.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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DISCUSSION:

A rather unusual severe weather setup as a low pressure system rides along a frontal boundary that is NW-SE oriented from central OH into central MD. Warm-sector instability on the order of 500-1000+ J/kg SBCAPE will develop over WV and western VA during the afternoon, which will help initiate a few areas of showers and storms. A convergence area over the Appalachians will help trigger storms early, with better instability upstream ahead of the southward-moving cold front that will move through OH and WV during the late afternoon and early evening. Things will look a little messy on radar at first, but eventually some strong/severe cells will form in the westernmost parts of the region. The main threat from these storms will be hail and wind damage, with an isolated threat for a few tornadoes. Speed shear is good with this system, but winds will be largely unidirectional, which will hinder tornadic development. Upper-levels are somewhat favorable as left-exit region divergence and some support from the 500mb vort. provide good synoptic lift.

As these storms push east into the Apps. and coastal plain, they will likely lose some intensity as the surface instability wanes. However, elevated instability should be sufficient to maintain thunderstorms with hail (maybe severe) and gusty winds (likely not severe) as the storms reach the DC/BWI region in the early evening. Depending on the amount of the elevated CAPE, storms could maintain themselves rather well and provide the area with a good lightning show.

Chase-wise, I’m considering taking I-68 to Morgantown, WV and then waiting to see where storms initiate. Should storms end up more favorable to the south, it will be a quick drive on I-79 towards Charleston, WV to get into better position.

-----

And just for record-keeping here's the Day 2 update from the SPC:

day2probotlk_20110322_1730_any_prt.gif

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DISCUSSION:

A rather unusual severe weather setup as a low pressure system rides along a frontal boundary that is NW-SE oriented from central OH into central MD. Warm-sector instability on the order of 500-1000+ J/kg SBCAPE will develop over WV and western VA during the afternoon, which will help initiate a few areas of showers and storms. A convergence area over the Appalachians will help trigger storms early, with better instability upstream ahead of the southward-moving cold front that will move through OH and WV during the late afternoon and early evening. Things will look a little messy on radar at first, but eventually some strong/severe cells will form in the westernmost parts of the region. The main threat from these storms will be hail and wind damage, with an isolated threat for a few tornadoes. Speed shear is good with this system, but winds will be largely unidirectional, which will hinder tornadic development. Upper-levels are somewhat favorable as left-exit region divergence and some support from the 500mb vort. provide good synoptic lift.

As these storms push east into the Apps. and coastal plain, they will likely lose some intensity as the surface instability wanes. However, elevated instability should be sufficient to maintain thunderstorms with hail (maybe severe) and gusty winds (likely not severe) as the storms reach the DC/BWI region in the early evening. Depending on the amount of the elevated CAPE, storms could maintain themselves rather well and provide the area with a good lightning show.

Chase-wise, I’m considering taking I-68 to Morgantown, WV and then waiting to see where storms initiate. Should storms end up more favorable to the south, it will be a quick drive on I-79 towards Charleston, WV to get into better position.

-----

And just for record-keeping here's the Day 2 update from the SPC:

Glad to have you over this way. Just some advice, I would stick to the interstate as long as possible in the central part of the state. Once you get off, the roads twist around so much you won't tell what direction you're looking at, you won't see much unless you're on top of a hill, and the cell coverage sucks.

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Hmm.... looks like storms could fire a little earlier than expected locally, though they'd still be elevated. It would be nice to play the convergence zone in VA since we wouldn't have to worry about the mountains, but the overall instability will likely not be as good as the air just ahead of the cold front.

EDIT: GFS parameters look better than the NAM for central+northern VA... will depend on strength of low-level WAA to bring the warm sector further north.

Lots of disagreement still with this one... Nowcasting FTW.

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hatched hail area extending into much of West Virginia

The SPC discussion was about as bullish on hail as I've ever seen lol

Can't read it now (time for work!), but it's elating to see them upgrade it to a Moderate Risk with 5% TOR risk (with the 45% hatched hail and 30% wind). NoVA and most of MD now included in the Slight!

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Just an fyi...the area around the Flatwoods exit 67 on I-79 opens up where you can see far off if you get down that way.

Not sure if we'll make it that far south... multiple hi-res models showing a nice area of convection between Clarksburg up to around Washington, PA going into the early evening. That's kind of what I was hoping to catch. Thanks for the information regardless... always helps to get terrain info. out in that area.

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Not much change with the 13z update... here's some interesting discussion:

...OH/TN VALLEYS EWD TO THE ATLANTIC COAST THROUGH TONIGHT...

A SWATH OF 55-60 F BOUNDARY LAYER DEWPOINTS IS SPREADING NEWD FROM

MS/AL/TN/AR TOWARD THE OH VALLEY ON A 40-50 KT WSWLY LLJ. THIS

MOISTURE WILL COMBINE WITH DAYTIME HEATING AND 8 C/KM MIDLEVEL LAPSE

RATES N OF THE JET CORE TO SUPPORT MODERATE INSTABILITY /MLCAPE

VALUES AROUND 1500 J PER KG/ IN THE WARM SECTOR THIS AFTERNOON.

CONVECTIVE INHIBITION WILL WEAKEN BY MIDDAY OVER A RATHER BROAD

AREA...AND MULTIPLE BANDS OF THUNDERSTORMS ARE EXPECTED TO DEVELOP

BY EARLY AFTERNOON. THOUGH LOW-LEVEL FLOW IS EXPECTED TO WEAKEN

SOME AND VEER TO MORE WLY DURING THE DAY...DEEP-LAYER VERTICAL SHEAR

AND STRAIGHT HODOGRAPHS WILL BE FAVORABLE FOR BOTH SPLITTING

SUPERCELLS AND FAST-MOVING LINE SEGMENTS.

THE COLD MIDLEVEL TEMPERATURES /NEAR -20 C AT 500 MB/...STEEP LAPSE

RATES...AND SUPERCELL WIND PROFILES APPEAR SUPPORTIVE OF A

RELATIVELY WIDESPREAD THREAT FOR LARGE HAIL...SOME OF WHICH COULD BE

SIGNIFICANT. DAMAGING WINDS CAN ALSO BE EXPECTED AS A RESULT OF

HIGH MOMENTUM /35-50 KT/ FLOW IN THE LOWEST FEW KM AGL...IN

COMBINATION WITH STEEP LOW-LEVEL LAPSE RATES. THE TORNADO THREAT IS

LESS CERTAIN GIVEN THE LIMITED LOW-LEVEL HODOGRAPH CURVATURE...BUT A

FEW TORNADOES WILL STILL BE POSSIBLE GIVEN THE LIKELIHOOD OF

MULTIPLE SUPERCELLS OVER A BROAD AREA THIS AFTERNOON/EVENING.

THUNDERSTORMS WILL ALSO SPREAD E OF THE APPALACHIANS LATE THIS

AFTERNOON INTO TONIGHT AS THE SYNOPTIC SYSTEM PROGRESSES EWD/ESEWD.

STRONG WIND PROFILES WILL CONTINUE...BUT LESSER INSTABILITY COMPARED

TO AREAS W OF THE MOUNTAINS SHOULD RESULT IN A GRADUAL LESSENING OF

THE DAMAGING WIND/HAIL THREAT OVERNIGHT TOWARD THE ATLANTIC COAST.

THE SRN EXTENT OF THE SEVERE STORM THREAT IS SOMEWHAT UNCERTAIN.

DEEP-LAYER VERTICAL SHEAR WILL BE VERY STRONG BENEATH THE JET CORE

AS FAR S AS NRN AL...WHERE BOUNDARY LAYER DEWPOINTS SHOULD REMAIN

NEAR 60 F. MIDLEVEL LAPSE RATES WILL BE MUCH LESS FAVORABLE

COMPARED TO AREAS FARTHER N...ON THE CYCLONIC SIDE OF THE JET...AND

THIS WILL LIMIT CAPE. STILL...THE STRONG WIND PROFILES AND

SUBSTANTIAL LOW-MIDLEVEL BUOYANCY COULD SUPPORT STORMS WITH DAMAGING

WINDS.

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In regards to elevated instability, is there usually a hail limit as to how large the hail is that the storms can produce? For example, if a storm in WV in the unstable airmass is producing ping pong sized hail and it moves into an elevated instability airmass... will it keep that sized hail or will it slowly weaken? I hope my question makes sense

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In regards to elevated instability, is there usually a hail limit as to how large the hail is that the storms can produce? For example, if a storm in WV in the unstable airmass is producing ping pong sized hail and it moves into an elevated instability airmass... will it keep that sized hail or will it slowly weaken? I hoe my question makes sense

I would think it would weaken but pea to nickel sized hail would remain possible. This is obviously not a scientific answer.

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CRW's Disco... Severe to occur later this afternoon after this first batch moves through late morning.

NAM/GFS/HRRR MODELS INDICATE AN AREA OF SHOWERS/STORMS WILL DEVELOP TO

OUR WEST LATER THIS MORNING...AND THEN MOVE EAST THRU THE LATE MORNING

HOURS. IN ITS WAKE...THE AIRMASS IS EXPECTED TO RECOVER INTO THE

AFTERNOON HOURS. WHILE THE AIRMASS WILL BECOME UNSTABLE...MODELS

SOUNDINGS SUGGEST THERE WILL BE A MID-LEVEL CAP.

THE COMBINATION OF DAYTIME HEATING AND UPPER LEVEL FORCING ASSOCIATED

WITH FEATURE APPROACHING FROM THE WEST SHOULD RESULT IN THE CAP

BREAKING AND THUNDERSTORMS DEVELOPING.

SPC HAS A MODERATE RISK FOR SEVERE THUNDERSTORMS THIS AFTERNOON

AND EVENING. APPEARS LARGE HAIL AND DAMAGING WINDS WILL BE THE

MAIN THREAT. THEY EVEN INDICATE THAT SOME OF THE STORMS COULD BE

PARTICULARLY DAMAGING WITH LARGE AMOUNTS OF HAIL.

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