#278 Postby weatherdude1108 » Wed Jun 19, 2019 3:28 pm
Looks like it could be an active period this evening/tonight for you all north Texas.
Mesoscale Discussion 1136
NWS Storm Prediction Center Norman OK
0314 PM CDT Wed Jun 19 2019
Areas affected...Northern Texas...far southern Oklahoma...southwest
Arkansas...and far northwest Louisiana
Concerning...Severe potential...Watch likely
Valid 192014Z - 192245Z
Probability of Watch Issuance...95 percent
SUMMARY...Storm development is expected by late afternoon/early
evening. A watch is likely.
DISCUSSION...Low-level southerly flow around 10 to 15 knots
continues to advect high theta-e air northward across central and
northern Texas in the wake of last night's MCS. A cumulus field has
expanded and advected northward on the northern extent of this
moisture rich air mass. The 19Z FWD RAOB suggests the air mass has
mostly recovered from earlier convective overturning with deep
boundary layer moisture and very steep mid-level lapse rates (~8.5-9
C/km) with dewpoints in the mid 70s and temperatures in the low 90s.
This combination of a high theta-e air mass beneath very steep
mid-level lapse rates has led to an extremely unstable air mass with
MLCAPE around 4000 to 4500 J/kg. CINH has been mostly eroded now
across this area with less than 50 J/kg on the 19Z FWD sounding.
Surface streamline analysis shows the strongest low-level confluence
just north of Abilene in the vicinity of an analyzed 1004hPa surface
low as of 19Z. Initial convective development may occur in this area
as early as 21Z where both buoyancy and mesoscale forcing will be
most supportive. Additional storms may form eastward along the
instability gradient as surface temperatures approach the convective
temperature. In fact, recent 1-min GOES16 imagery shows some deeper
towering cumulus development along what appears to be the remnant
outflow boundary from the overnight MCS which is now lifting north.
Any storms which develop should quickly take on supercell structures
given the extreme instability and effective shear around 50 to 60
knots (57 kts FWD 19Z RAOB).
Initial storms will pose the greatest threat for very large hail and
a few tornadoes while storm mode remains discrete. Weak low-to-mid
tropospheric flow will be a limiting factor to a greater tornado
threat with the strengthening and elongating low-level hodograph not
materializing until after 00Z once storm mode becomes less discrete.
However, there is enough low-level cyclonic curvature in the lowest
1 to 2 km to support the potential for a few tornadoes.
The environmental variables are very supportive for very large hail,
including the potential for giant hail given the extreme
instability, very steep mid-level lapse rates, and >50 kts effective
shear. The only negative factor to a more widespread threat for
giant hail will be the limited duration of a more discrete storm
mode.
Widespread storm coverage is expected between 00Z and 03Z due to the
arrival of the mid-level shortwave trough and a strengthening
low-level jet. A very large hail threat will remain for a few hours
before the primary threat becomes damaging wind as storms congeal.
There is significant wind gust potential given the extreme
instability and the the steep mid-level lapse rates with the
potential for wind-driven large hail, especially in the 01-04Z
timeframe.
..Bentley/Guyer.. 06/19/2019
Last edited by
weatherdude1108 on Wed Jun 19, 2019 3:29 pm, edited 1 time in total.
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