SPC MD 120



MD 0120 CONCERNING SEVERE POTENTIAL…WATCH POSSIBLE FOR CENTRAL INTO NORTHERN MISSISSIPPI

MD 0120 Image

Mesoscale Discussion 0120
NWS Storm Prediction Center Norman OK
0146 PM CST Wed Feb 12 2020

Areas affected...Central into northern Mississippi

Concerning...Severe potential...Watch possible 

Valid 121946Z - 122145Z

Probability of Watch Issuance...40 percent

SUMMARY...At least a few severe storms are possible in the next few
hours, going into early evening. Damaging wind gusts appear to be
the primary threat, though a couple of tornadoes cannot be ruled
out. Convective trends are being monitored for the need of a WW.

DISCUSSION...A well defined mid-level trough continues to approach
the southeast states, with a broad low-level mass response promoting
moistening of the low-levels (i.e. a northward surge of upper 60s to
near 70 F dewpoints), particularly across LA into central MS. In
addition, breaks in the clouds from central MS southward have
allowed for some diurnal heating, with temperatures warming into the
mid 70s. Nonetheless, given the overall cloudy conditions, and poor
mid-level lapse rates (mainly under 6 C/km based on latest
mesoanalysis and the latest RAP forecast soundings) across the warm
sector, overall instability is expected to be mediocre. MLCAPE is
expected to be maximized in the 500-1000 J/kg range, and confined
within tall, skinny vertical profiles. As such, robust convection is
expected to be relatively sparse in nature.

Still, deep-layer/low-level speed shear (40+ knots in the 0-1 km
layer) is prevalent across the warm sector, with long, curved
hodographs depicting a favorable kinematic environment for
organized, rotating storms. Flow above 1 km however, appears to be
unidirectional. With deep-layer winds bearing a strong parallel
component of flow to the approaching cold front, much of the
convection is expected to be linear in nature. While a forced line
of convection is expected, the strong low-level speed shear and
modest directional shear (yielding over 400 m2/s2 effective SRH) may
promote the development of a couple of tornadoes, where QLCS
circulations may coincide axes of locally higher buoyancy.

All 12Z HREF members initiate a squall line along the cold front by
20-22Z, though the trend among the latest HRRR runs show less
vigorous convection overall. Given the aforementioned limitations to
the thermodynamic environment and associated weakening trends among
model guidance, confidence in the necessity of a WW issuance remains
modest at this time. Trends will continue to be monitored for a WW
issuance.

..Squitieri/Thompson.. 02/12/2020

...Please see www.spc.noaa.gov for graphic product...

ATTN...WFO...BMX...HUN...MEG...JAN...

LAT...LON   32269094 33559000 34458906 35008815 34938776 34798760
            34478752 33938760 33238790 32558825 32308856 32068914
            31949028 32269094 

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