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April 7th-10th Severe Weather


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I think the one thing that would keep them from issuing the day 3 moderate is the unknown exact timing of the surface front/dryline. Some pretty big differences just between the GFS and NAM alone. They may just broad brush a wide region with a hatched high-end slight for now until timing becomes more clear. Otherwise it's looking pretty likely that a widespread severe weather episode is likely for that period.

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I'm not really relying on it, just commenting. But you can't tell me that the VV charts don't take on a more linear look between 00z-06z Monday.

I really don't. Given the wind profiles and late/intense rapid height falls and late cap erosion/fracture and what will likely be even greater instability it would likely be a line of discretely initiating supercells. It looks linear in the VV's--but even if you look at GFS qpf you can see it isn't simulating a squall line.

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I think the one thing that would keep them from issuing the day 3 moderate is the unknown exact timing of the surface front/dryline. Some pretty big differences just between the GFS and NAM alone. They may just broad brush a wide region with a hatched high-end slight for now until timing becomes more clear. Otherwise it's looking pretty likely that a widespread severe weather episode is likely for that period.

Doesn't a hatch lend to a MDT on day 3?

http://www.spc.noaa.gov/misc/SPC_probotlk_info.html

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I really don't. Given the wind profiles and late/intense rapid height falls and late cap erosion/fracture and what will likely be even greater instability it would likely be a line of discretely initiating supercells. It looks linear in the VV's--but even if you look at GFS qpf you can see it isn't simulating a squall line.

Mode (particularly how long things remain discrete) is anybody's guess right now and like usual we probably won't know for sure until it's happening.

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I'm not really relying on it, just commenting. But you can't tell me that the VV charts don't take on a more linear look between 00z-06z Monday.

I agree with baroclinic_instability that you can't really look at the model output VVs and determine convective mode from that. I've seen plenty of times when the VVs "looked linear", but the shear profiles were obviously supportive for discrete supercells. In this particular case, it might be pretty linear, given that the directional shear is pretty borderline, but it's tough to tell.

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I agree with baroclinic_instability that you can't really look at the model output VVs and determine convective mode from that. I've seen plenty of times when the VVs "looked linear", but the shear profiles were obviously supportive for discrete supercells. In this particular case, it might be pretty linear, given that the directional shear is pretty borderline, but it's tough to tell.

Fair enough. At this point I am leaning toward more of a QLCS by the time it gets here but I'd love for the knowledgeable folks to keep chiming in.

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Going to be a busy weekend, concur with the other met's here. I don't know if the tornado threat will evolve much past an area around the initiation zone, but the more discrete these storms stay would certainly lend to lingering that threat. And any little boundaries lifting north from the late Saturday Night stuff will lend to potential of some locally backed winds Sunday perhaps over IL/WI. There is going to be tremendous instability so these things will just explode once they go. Damaging wind threat I think may end up being the real story with this set up.

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DAY 1 CONVECTIVE OUTLOOK

NWS STORM PREDICTION CENTER NORMAN OK

1227 AM CDT FRI APR 08 2011

VALID 081200Z - 091200Z

...THERE IS A SLGT RISK OF SVR TSTMS ACROSS PORTIONS OF THE OH/TN

VALLEY INTO SRN MO...

...MID MS/OH/TN VALLEY REGION...

ASIDE FROM A PSEUDO-STATIONARY FRONTAL ZONE DRAPED ACROSS THE OH

VALLEY INTO MO...A RATHER NONDESCRIPT LARGE SCALE PATTERN WILL BE

SITUATED ACROSS THE REGION FRIDAY WITH WEAK HEIGHT RISES EXPECTED

THROUGH THE PERIOD. WEAK LARGE SCALE FORCING THROUGH THE AFTERNOON

HOURS WILL ENSURE THE SIGNIFICANCE OF THE AFOREMENTIONED SFC

BOUNDARY IN REGARDS TO ORGANIZED THUNDERSTORM DEVELOPMENT. LATEST

MODEL GUIDANCE SUGGEST STRONG BOUNDARY LAYER HEATING WILL BE NOTED

ACROSS SRN IL INTO NRN KY/SRN OH. THIS SHOULD ENHANCE THE PROSPECT

FOR CONVECTIVE DEVELOPMENT WITHIN STRONGLY SHEARED ENVIRONMENT

FAVORABLE FOR SUSTAINED ROTATING UPDRAFTS. FORECAST SOUNDINGS FAVOR

SUPERCELL DEVELOPMENT EARLY IN THE CONVECTIVE CYCLE AND THIS SEEMS

REASONABLE GIVEN THE WEAK FORCING. WITH TIME STORM MERGERS AND

CONVECTIVE INTERFERENCE COULD LEAD TO STORM CLUSTERS AS MEAN WIND

VECTOR DRIVES TSTMS SEWD AT ROUGHLY 30KT. FOR THIS REASON IT

APPEARS THERE WILL BE A THREAT FOR LARGE HAIL...DAMAGING WINDS AND

PERHAPS EVEN A FEW TORNADOES AS BOUNDARY LAYER MOISTURE AND RH

VALUES WILL HAVE RISEN SIGNIFICANTLY BY THIS TIME.

FARTHER WEST ACROSS MO...IT/S NOT ENTIRELY CLEAR HOW MUCH DIURNAL

ACTIVITY WILL DEVELOP ALONG THE FRONT AS LOW LEVEL CONVERGENCE WILL

BE ESPECIALLY WEAK ACROSS THIS REGION. HOWEVER...LLJ SHOULD

INCREASE MARKEDLY NEAR SUNSET INTO THE EVENING HOURS. STRONG WARM

ADVECTION ACROSS THIS REGION WILL LIKELY FORCE A BOUT OF SEVERE

THUNDERSTORMS AFTER DARK THAT WILL EVOLVE WITHIN A VERY UNSTABLE

ENVIRONMENT CHARACTERIZED BY STEEP LAPSE RATES AND MUCAPE

APPROACHING 2000-3000 J/KG. LARGE HAIL IS CERTAINLY POSSIBLE IF

ACTIVITY CAN BECOME SUSTAINED BENEATH THE LLJ ACROSS THIS REGION.

...TX/OK...

STRONG DIURNAL HEATING WILL ONCE AGAIN BE NOTED ACROSS THE SRN

PLAINS...ESPECIALLY ALONG/WEST OF THE DRYLINE. UNCAPPED THERMALS

NEAR THE DRYLINE WILL LIKELY STRUGGLE TO SUSTAIN THEMSELVES WITHIN A

RIDGY MID LEVEL ENVIRONMENT. HOWEVER...SIGNIFICANT MOISTENING

WITHIN THE BOUNDARY LAYER AND WEAK LOW LEVEL CONVERGENCE MAY RESULT

IN ONE OR TWO SEVERE THUNDERSTORMS NEAR 09/00Z. IF STORMS MANAGE TO

INITIATE LARGE HAIL AND DAMAGING WINDS COULD OCCUR. THIS ACTIVITY

SHOULD DISSIPATE WITHIN A FEW HOURS AS BOUNDARY LAYER COOLS.

...GULF STATES...

EARLY EVENING WV IMAGERY SUGGESTS A WEAK UPPER VORT/SHORTWAVE TROUGH

IS EJECTING NEWD ACROSS MEXICO INTO DEEP SOUTH TX. THIS FEATURE MAY

NOT BE HANDLED WELL WITHIN BROADER HEIGHT RISES THAT SHOULD

OVERSPREAD THE SRN STATES LATER TODAY. AS A RESULT...WEAK ASCENT

MAY ENHANCE THE PROSPECT FOR ISOLATED THUNDERSTORMS ALONG THE ERN

PLUME OF STEEPER LAPSE RATES...ESPECIALLY ACROSS AL INTO GA. IF

SO...STRONG SHEAR AND SUBSTANTIALLY MORE MOIST/UNSTABLE AIRMASS WILL

BE IN PLACE FOR POSSIBLE SEVERE. WILL MAINTAIN LOW PROBS FOR

WIND/HAIL PRIMARILY DUE TO THE SUBTLE SHORTWAVE AND WEAK FORCING.

HOWEVER IF IT APPEARS A MORE ORGANIZED CONVECTIVE SCENARIO WILL

UNFOLD THEN A SLIGHT RISK MAY BE REQUIRED.

..DARROW/HURLBUT.. 04/08/2011

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A serious increase in instability in northern IL this run...some places had near 1000 j/kg of CAPE on the 12z NAM and now its showing near 3500 j/kg on this run and actually all the CIN erased but no precip breaks out either INVOF the warm front or on the dryline.

That's because there is either no VA (GFS) or AVA (NAM) across N IL Saturday. No lift.

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day2.prob.gif

629

ACUS02 KWNS 080542

SWODY2

SPC AC 080541

DAY 2 CONVECTIVE OUTLOOK

NWS STORM PREDICTION CENTER NORMAN OK

1241 AM CDT FRI APR 08 2011

VALID 091200Z - 101200Z

...THERE IS A SLGT RISK OF SVR TSTMS ACROSS PARTS OF THE SRN

PLAINS...CNTRL PLAINS AND UPPER MIDWEST...

...THERE IS A SLGT RISK OF SVR TSTMS ACROSS PARTS OF THE OH

VALLEY...SRN APPALACHIAN MTNS AND CAROLINAS...

..SRN AND CNTRL PLAINS/UPPER MIDWEST

AN UPPER-LEVEL TROUGH OVER THE INTERMOUNTAIN WEST IS FORECAST TO

MOVE INTO THE FOUR CORNERS REGION SATURDAY. WELL AHEAD OF THE

SYSTEM...A LOW-LEVEL JET WILL STRENGTHEN IN THE SCNTRL STATES. THIS

WILL HELP TO ESTABLISH A BROAD MOIST AXIS ACROSS THE GREAT PLAINS

AND MS VALLEY WHERE MODERATE INSTABILITY APPEARS LIKELY TO DEVELOP

SATURDAY AFTERNOON. AS A WELL-DEVELOPED MID-LEVEL JET MOVES OUT INTO

THE CNTRL PLAINS...THUNDERSTORMS APPEAR MOST LIKELY TO DEVELOP IN

THE EXIT REGION OF THE JET ACROSS THE MID-MO VALLEY SATURDAY

AFTERNOON SPREADING NEWD ACROSS THE UPPER MIDWEST SATURDAY EVENING.

THUNDERSTORMS ALSO MAY DEVELOP SWD ALONG A DRYLINE SATURDAY EVENING

FROM CNTRL KS INTO WRN OK AND NW TX.

THE MID-LEVEL JET SHOULD RESULT IN A STRONGLY SHEARED ENVIRONMENT

ACROSS MOST OF THE GREAT PLAINS AND UPPER MIDWEST MAKING CONDITIONS

FAVORABLE FOR SEVERE THUNDERSTORMS. AN ENHANCED SEVERE THREAT MAY

DEVELOP FROM NE KS NNEWD ACROSS ERN NEB...IA AND SRN MN WHERE

CONVECTIVE COVERAGE IS EXPECTED TO BE GREATER SATURDAY EVENING. A

FEW TORNADOES...LARGE HAIL AND WIND DAMAGE WILL BE POSSIBLE WITH THE

MORE ORGANIZED CELLS. THE SHEAR ENVIRONMENT SHOULD SUPPORT SUPERCELL

DEVELOPMENT ESPECIALLY IN AREAS WITH THE STRONGEST INSTABILITY AND

AN ISOLATED VERY LARGE HAIL THREAT MAY DEVELOP FROM ERN NEB NEWD

INTO SW WI. THE SEVERE THREAT ALONG THE DRYLINE SHOULD BE

INCREASINGLY ISOLATED WITH SWD EXTENT BUT HAIL AND WIND DAMAGE WILL

ALSO BE POSSIBLE THERE.

..OH VALLEY/SRN APPALACHIAN MTNS/CAROLINAS

AN UPPER-LEVEL RIDGE IS FORECAST TO BE IN PLACE ACROSS THE ERN

STATES SATURDAY WITH NWLY FLOW LOCATED FROM THE SRN APPALACHIAN MTNS

SEWD ACROSS THE CAROLINAS. MODERATE INSTABILITY SHOULD EXIST FROM

THE OH VALLEY SEWD INTO THE CAROLINAS WHERE SCATTERED THUNDERSTORMS

SHOULD INITIATE AROUND MIDDAY SATURDAY. FORECAST SOUNDINGS SATURDAY

AFTERNOON ALONG THIS CORRIDOR SHOW MODERATE TO STRONG DEEP LAYER

SHEAR PROFILES WITH SOME DIRECTIONAL SHEAR SUGGESTS CONDITIONS WILL

BE FAVORABLE FOR SEVERE STORMS. SFC DEWPOINTS IN THE MID TO UPPER

60S F AND STEEP LOW-LEVEL LAPSE EVIDENT ON FORECAST SOUNDINGS WOULD

BE SUFFICIENT FOR A WIND DAMAGE THREAT. IF SUPERCELLS CAN

ORGANIZE...THEN AN ISOLATED TORNADO THREAT AND HAIL THREAT WILL ALSO

BE POSSIBLE.

..BROYLES.. 04/08/2011

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Nam is going insane with elevated parameters overnight Saturday night.

Almost 3000 J/kg of elevated instability, sure there is an inversion, but that is some big time hail potential. With excellent shear too.

Some very good severe parameters there (showalter/sweat/TT)

post-55-0-87969000-1302241487.jpg

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That's because there is either no VA (GFS) or AVA (NAM) across N IL Saturday. No lift.

Synoptic scale ascent is only a small part of it though. And since I like to argue synoptics (I am just messing here), should we be making use of synoptic forcings and the QG Theory of synoptic motion--it should always be differential vorticity advection :)

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