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June 5th-September 1st, 2023 | Severe Storm Sequence


Iceresistance

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14 minutes ago, Neoncyclone said:

Matador, TX has some very bad damage. this supercell in Texas is absolutely massive!

 

Screenshot_20230621_224042_RadarScope.jpg

100mph winds and softball sized hail. No thanks!

Quote
Severe Weather Statement
National Weather Service San Angelo TX
1042 PM CDT Wed Jun 21 2023

TXC151-220400-
/O.CON.KSJT.TO.W.0020.000000T0000Z-230622T0400Z/
Fisher TX-
1042 PM CDT Wed Jun 21 2023

...A TORNADO WARNING REMAINS IN EFFECT UNTIL 1100 PM CDT FOR FISHER
COUNTY...

At 1041 PM CDT, a severe thunderstorm capable of producing a tornado
was located over Rotan, moving south at 40 mph. This storm also has
a history of producing over 100 mph winds and up to softball size
hail.

HAZARD...Tornado and softball size hail.

SOURCE...Radar indicated rotation.

IMPACT...Flying debris will be dangerous to those caught without
         shelter. Mobile homes will be damaged or destroyed. Damage
         to roofs, windows, and vehicles will occur.  Tree damage is
         likely.

This dangerous storm will be near...
  Roby around 1055 PM CDT.
  Sylvester around 1100 PM CDT.
  Longworth around 1105 PM CDT.

Other locations impacted by this tornadic thunderstorm include Busby,
Capitola and Us-180 Near The Fisher-Scurry County Line.

 

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24 minutes ago, StormfanaticInd said:

Watching Sunday. Spc mentioned the Ohio Valley in their extended outlook 

Temperatures should
then quickly rebound and warm up into the weekend as warm air
advection increases from the west.

The warm air advection is driven by a developing low over the
Plains, which will slowly move northeastward allowing the Rex Block
to break down. This system will make its way towards Indiana by
Sunday, allowing for shower and storm chances to return. There are a
few questions that remain with this system, and how things play out
as it passes through. One question is how any potential upstream
convection on Saturday may evolve. If it were to develop into an
MCS, it may progress towards Indiana on the back of a rather robust
jet streak. Warm moist advection ahead of it, along with a potent
low-level jet, may allow it to survive into the morning hours on
Sunday. This would then lead to the next question, if this system
were to survive into Indiana for Sunday...how would that affect
convective development that afternoon? The system could end up
stabilizing the atmosphere sufficiently to limit the convective
threat later in the day. Should the MCS not develop, we`ll likely be
left with a more pristine environment for afternoon convective
development. Current guidance, while not in total agreement, shows
enough shear for convective organization...so the potential for
severe weather will need to be watched. A third question is timing,
if the system passes through too fast or too slow, that will of
course affect which locations are favored for subsequent convective
development. Overall, a lot need to be watched and trends will be
monitored closely.

Beyond this weekend, guidance hints at ridging redeveloping over
Texas with broad troughing remaining over the northeastern US. This
would place Indiana within a region of northwesterly flow aloft.
Additionally, southwesterly low-level flow may make a return during
this time as well. This is in contrast to the recent pattern
featuring northerly or northeasterly flow at the surface. Such a
pattern would be more conducive to upstream convective systems
propagating southeastward. This would be particularly true should a
northwest to southeast instability gradient develop over the region.
This would imply a southwest to northeast gradient in temperatures,
which is reflected in the current forecast through the middle part
of next week.

Ensembles are in rather good agreement regarding this pattern shift.
In fact, GEFS ensemble member spaghetti plots are not as messy as
they would normally be...clearly showing a ridge over Texas with
troughing over the northeastern US. The members only begin to
rapidly diverge towards the end of the month, with any discernible
signal disappearing by July 1st. ECMWF Ens likewise shows a similar
pattern evolution through the end of the month. Overall, confidence
in the broad synoptic scale pattern is greater than normal for this
period. Confidence is low regarding potential convective evolution
and MCS propagation, as these features depend on mesoscale forcing
and factors that are not resolvable at this range.
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Morning discussion from INDYimage.png.18ec3dbc6d1d31a5a4e5cac62f22c556.png

 

On the periphery of weak upper level ridging, Saturday will be dry
and warm across Central Indiana. This is not the case upstream, as a
developing low pressure over the Great Plains and shortwave upper
trough will trigger storms (and potentially an MCS) to develop out
closer to Iowa. Locally, the development of this surface low will
contribute to the breakdown of the past week`s block and will allow
surface flow to veer to westerly and southerly. This, in turn, will
enhance warm air advection over our forecast area, allowing
temperatures to warm into the upper 80s/lower 90s on Saturday. Low
level flow strengthens into Sunday, only enhancing this ongoing warm
air and moisture advection and setting the stage for potential
convective thunderstorm activity in Indiana.

While this system is likely to give our area the best rain chances
we have seen in a while, multiple questions remain up in the air
regarding any severe weather potential on Sunday. The first of these
questions relates to the upstream activity mentioned above; will it
develop into an MCS and will this MCS make it all the way to
Indiana? The presence of a seasonably potent 500mb jet streak nearby
depicted in some guidance on Sunday would support this system
sustaining itself. However, it will also have to overcome a loss of
diurnal thermal instability, as it would approach the area
overnight/early in the morning. The next question depends on the
strength of any lingering activity; would it locally suppress the
thermodynamic environment via latent heat processes and decrease
instability for Sunday afternoon? Weaker or nonexistent Sunday
morning storms would allow for greater potential for convective
initiation across Indiana later in the day. Any storms that form on
Sunday afternoon will exist in a favorable shear directional regime,
and modeled soundings demonstrate the need to monitor severe weather
approach if favorable thermodynamics are realized. More questions
exist regarding the spatiotemporal placement of the driving
shortwave trough; will the best forcing be displaced south or east
of the area? While guidance generally agrees in the shift towards a
more favorable synoptic pattern for convection (and rain!!), many of
these questions will remain up in air until the system enters the
range of higher-resolution modeling. Stay tuned to future forecast
updates as this event approaches, as trends in the above questions
will be watched in the coming days.
Edited by StormfanaticInd
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  • Meteorologist

Definitely some of the worst vehicle damage I have seen in a long time. 

I thought the Mississippi tornado could have been a low end EF-4 based on the wide spread tree damage, but I'm also not familiar with which trees there are weaker to winds. Matador has a lot more going for it for a violent tornado rating. The vehicle damage is at least on par with Rolling Fork and Mayfield. We don't have DIs for this kind of damage, but we can infer based on previous tornadoes on what likely occurred and use it to back up actual DIs

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ILN has a long write up concerning Sunday.

Quote
Midlevel ridging will /very briefly/ build into the region
Saturday night into early Sunday morning ahead of the next
system which will approach the OH Vly quickly from the W into
the afternoon hours Sunday. Synoptically, a deepening low
pressure center will track from the upper Midwest to the wrn
Great Lakes during the daytime Sunday, with the OH Vly
positioned in an area of increasing mid/upper level diffluence,
with a seasonably potent jetstreak fcst to wrap around the srn
periphery of the low center into the region by Sunday evening.
This will provide some mid/upper level support to initiate (or
possibly maintain) convection across the area as an
increasingly-favorable thermodynamic environment advects in from
the WSW.

There are several items to discuss as it relates to the setup
that should evolve Sunday afternoon into Sunday night. Although
there are still some timing and orientation differences to be
worked out, the overlap of favorable thermodynamics (LL- and
deep-layer instby) and kinematics (sufficient LL- and deep-layer
shear profiles and a sharp S/W) suggest a concerning setup for
strong/severe storms during this time period. Although the
gradual increase in broader-scale lift/forcing will undoubtedly
contribute to convective coverage/intensity as we progress into
the late afternoon/evening, there are admittedly still some
uncertainties in regards to early day activity/modulations to
the environment that just are not well- depicted at this time
range. There are several signals to suggest a well-formed MCS
may originate in the central plains (IA/vicinity) and dive to
the SE into the mid MS Rvr Vly and SW OH Vly into the predawn
hours Sunday morning (but stay off to the SW of the ILN FA).
This may have consequences (from a convective blowoff/debris
standpoint) on rate and degree of destabilization efforts
further E/NE into the ILN FA into Sunday afternoon/evening,
especially as that will be the /source/ region of the air moving
in locally. There are some uncertainties regarding whether that
overturned environment from off to our W/SW will advect into
the ILN FA or whether more robust/rapid LL destabilization can
take place as early as mid afternoon. Either way, do expect that
there will be substantial destabilization taking place by
Sunday late afternoon/early evening pretty much area-wide with
the concurrent advection in of higher LL theta-e air from the SW
and the arrival of a more stout EML from the W by the evening.
This should act to steepen the midlevel lapse rates and provide
more deeper-layer instby (SB/ML CAPE near/exceeding 2000 J/kg),
which, when combined with 35+ kts 0-6km shear, suggests an
active Sunday afternoon/night could be in store for parts of the
area. Given the signals in the data, including some of those
mentioned here, feel confident enough to include the mention of
strong/severe storms (with both strong/damaging straight- line
winds and large hail) in the HWO area-wide, although there are
admittedly a few uncertainties in the convective
evolution/placement/location during this period. We will
continue to monitor the evolution of the setup closely.

The convective activity should wane very late Sunday evening
into early Sunday night as the best overlap of forcing/instby
get shunted to the E/SE. Quite a bit of wraparound moisture will
pivot back in from the N during the daytime Monday, keeping
SCT/numerous SHRA in the fcst into Monday evening. With this
setup, expect that high temps will be substantially cooler
Monday afternoon than will be the case Sunday. Kept NBM
deterministic temps for now, but given the coverage of clouds
and SHRA activity during the daytime, fcst highs may be further
trimmed in subsequent fcst updates.

 

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Kinda surprised the slight isn't farther north. NAM appears to have most of the storms across IN/OH. They do say an upgrade to enhanced is very possible. Maybe a rare day 3 update this afternoon/evening?

Quote
  Day 3 Convective Outlook  
   NWS Storm Prediction Center Norman OK
   0230 AM CDT Fri Jun 23 2023

   Valid 251200Z - 261200Z

   ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS ACROSS PARTS OF
   THE MID MISSISSIPPI...OHIO AND TENNESSEE VALLEYS...

   ...SUMMARY...
   A severe threat will be likely across parts of the mid Mississippi,
   Ohio and Tennessee Valleys on Sunday. Large hail, wind damage and
   perhaps a couple tornadoes will be possible.

   ...Mid Mississippi, Ohio and Tennessee Valleys...
   An upper-level trough will move eastward across the north-central
   states on Sunday, as a 60 to 70 knot mid-level jet translates
   eastward across the mid Mississippi Valley. At the surface, a low
   will move into the western Great Lakes as a cold front advances
   southeastward into the mid Mississippi Valley. Ahead of the front,
   surface dewpoints in the low to mid 70s F will contribute to a
   corridor of moderate to strong instability by early afternoon from
   western Tennessee into central and northern Kentucky. During the
   afternoon, convection is forecast to first initiate on the northern
   edge of the stronger instability, with storms moving eastward across
   the Ohio Valley during the mid to late afternoon. Convective
   coverage should continue expanding across the region during the
   early evening, with a band of storms moving east-southeastward into
   the central Appalachians, and southeastward into the Tennessee
   Valley. MCS development will be possible across parts of the Ohio
   and Tennessee Valleys.

   The mid-level jet will move into the Ohio Valley during the
   afternoon, enhancing large-scale ascent and creating moderate
   deep-layer shear. NAM forecast soundings near Cincinnati during the
   late afternoon have 0-6 km shear in the 40 to 45 knot range with
   some directional shear present in the low levels. In addition,
   MLCAPE is forecast to peak in the 3000 to 4000 J/kg range. This
   combined with mid-level lapse rates near 7 C/km should be favorable
   for supercells with large hail. Hailstones greater than 2 inches in
   diameter will be possible. Wind damage will also possible with
   supercells and the more intense line segments. In addition, 0-3 km
   storm-relative helicity is forecast to increase into the 300 to 350
   m2/s2 range, suggesting that a tornado threat may also develop. The
   severe threat could be upgraded to Enhanced Risk in later outlooks,
   if model runs continue to show a greater coverage of severe threat
   Sunday afternoon and evening.

   Further to the west, a severe threat will also be possible in parts
   of the Ozarks Sunday afternoon. Although a potential will exist for
   isolated large hail and wind damage, weaker large-scale ascent and
   warm temperatures in the mid-levels should keep convective coverage
   more isolated.

   ..Broyles.. 06/23/2023

 

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ILN latest thoughts.

Quote
.LONG TERM /SATURDAY NIGHT THROUGH THURSDAY/...
A deepening low pressure system will be moving east across the upper
midwest on Saturday night ahead of a well defined upper level PV
anomaly for late June. Locally over the Ohio Valley, winds should
shift to the south with the deepening low in the Upper Midwest
overnight allowing moisture to start gradually increasing. Forecast
lows are in middle 60s.

The forecast gets more interesting on Sunday due to the possibility
of thunderstorms that could become strong to severe during the
afternoon. The synoptic setup features the previously mentioned deep
low (by late June standards) progressing eastward across Upper
Midwest and Great Lakes ahead of a strong, southeast-diving, PV
anomaly. A substantial push of instability (1500-2000+ J/kg) is at
least moderately likely to occur across the Ohio Valley during the
day due to a surge of theta-e air and an EML advecting in from the
southwest. Strong deep layer shear (>40 knots) should be present
along with veered low level hodographs ahead of an approaching
trough axis which may back surface winds further. By late afternoon,
the trough axis is expected to pivot through the area along with the
upper-level PV anomaly which should act as a focus for possible
storm initiation in the potentially potent kinematic and
thermodynamic environment south of the low. If no convection occurs
early on Sunday (none is expected at this time) or the forecast does
not change, all modes of severe weather may be possible on Sunday
afternoon with boundary-parallel deep shear appearing likely. CAMs
should help resolve finer scale details in the coming 24-48 hours.
For now, Sunday afternoon will need to be watched as highlighted by
the HWO and SPC outlooks. Forecast highs reach into the middle to
upper 80s.

The chance for thunderstorms decreases quickly Sunday night when the
aforementioned trough axis moves east before increasing again on
Monday into Tuesday when the actual cold front moves through.
Temperatures drop below average behind the front by midweek and dry
weather returns.

 

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