Feb 26, 2018 1300 UTC Day 1 Convective Outlook
Updated: Mon Feb 26 12:34:11 UTC 2018 (20180226 1300Z Day 1 shapefile | 20180226 1300Z Day 1 KML)
Probabilistic to Categorical Outlook Conversion Table
Categorical Graphic
20180226 1300 UTC Day 1 Outlook Graphic
Day 1 Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
No Risk Areas Forecast
Probabilistic Tornado Graphic
20180226 1300 UTC Day 1 Tornado Probabilities Graphic
Probability of a tornado within 25 miles of a point.
Hatched Area: 10% or greater probability of EF2 - EF5 tornadoes within 25 miles of a point.
Day 1 Tornado Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
No Risk Areas Forecast
Probabilistic Damaging Wind Graphic
20180226 1300 UTC Day 1 Damaging Wind Probabilities Graphic
Probability of damaging thunderstorm winds or wind gusts of 50 knots or higher within 25 miles of a point.
Hatched Area: 10% of greater probability of wind gusts 65 knots or greater within 25 miles of a point.
Day 1 Wind Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
No Risk Areas Forecast
Probabilistic Large Hail Graphic
20180226 1300 UTC Day 1 Large Hail Probabilities Graphic
Probability of hail 1" or larger within 25 miles of a point.
Hatched Area: 10% or greater probability of hail 2" or larger within 25 miles of a point.
Day 1 Hail Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
No Risk Areas Forecast
   SPC AC 261234

   Day 1 Convective Outlook  
   NWS Storm Prediction Center Norman OK
   0634 AM CST Mon Feb 26 2018

   Valid 261300Z - 271200Z

   ...NO SEVERE THUNDERSTORM AREAS FORECAST...

   ...SUMMARY...
   Thunderstorms are possible across portions of the Southeast and Gulf
   Coast, deep south Texas, and parts of central/western California.

   ...Synopsis...
   In mid/upper levels, a strong shortwave trough -- now evident in
   moisture-channel imagery just offshore from the OR/CA border -- is
   expected to dig southeastward down the CA coast this period.  A
   closed 500-mb cyclone will develop near the SFO-MRY corridor and in
   the 00-06Z time frame, and should intensify as it moves over the
   Coast Range west of BFL by 12Z.  Associated large-scale
   ascent/cooling aloft will contribute weak convective instability in
   support of general thunderstorm potential over parts of
   northern/central CA this afternoon and evening.

   Downstream from this feature, westerly to southwesterly flow will
   prevail over most of the country.  Within that flow, the main
   perturbation should be a positively tilted shortwave trough -- much
   weaker than the one near the West Coast -- currently located from
   Lower MI across the Ozarks to northeast TX.  This trough should move
   east-northeastward and weaken through the period, reaching
   southeastern New England, DE, and western NC by 00Z, before moving
   offshore entirely.

   At the surface, 11Z analysis showed a diffuse cold front from the
   central/southern Appalachians across parts of southern MS,
   southeastern LA, and the northwestern Gulf, to near BRO.  The front
   should drift southward over the northwestern Gulf before stalling
   this afternoon and evening, while proceeding eastward over the
   southeast.  A weak prefrontal low was analyzed near PNS, and near
   the intersection of two outflow boundaries:  an older boundary
   extending across the AAF and JAX areas, and fresher outflow from
   ongoing convection/precip over southwestern GA, southeastern AL and
   extreme southeastern LA.  This low, associated with the mid/upper
   perturbation, is expected to move east-northeastward today, likely
   into rain-cooled air.

   ...Southern GA/northern FL Panhandle region...
   A southwest/northeast-aligned plume of convective precip, with
   sporadic, isolated, embedded thunderstorms, should proceed eastward
   across the region through mid-afternoon.  This activity is ahead of
   the bulk of overnight model progs, including even the shorter-fused,
   radar-assimilating, convection-allowing guidance.

   Somewhat favorable CAPE/shear parameter-space juxtapositions have
   been apparent in some models for 15Z-20Z.  In the boundary layer, a
   small wedge of optimal Gulf marine-sector air may advect into this
   region as the older/southern outflow boundary diffuses and moves
   northeastward, merging with the northern boundary, the surface low
   proceeds obliquely inland, and the related isallobaric forcing veers
   the maritime/tropical sector flow to southwesterly.  Forecast
   soundings from those most-aggressive progs depict 150-200 J/kg
   effective SRH near the combined boundary, along with around 45 kt
   southwesterly effective-shear vectors and around 500 J/kg MLCAPE. 
   However, caveats precluding an outlook are:

   1.  Ongoing convective trends showing decidedly subsevere/
   quasi-linear mode.  Given the weakening/positively tilted nature of
   the parent perturbation and its effects on flow geometry aloft,
   rendering mean winds nearly parallel to the convective plume, modal
   recovery is not very probable.
   2.  The presence of more antecedent precip, both east of the main
   line and in the line's faster/more eastward position as noted above.
    This renders uncertainty to extent of both prefrontal boundary
   retreat inland and diurnal/diabatic destabilization, especially
   given very weak lapse rates aloft per 12Z TLH sounding.
   3.  The veering itself south of the ultimately combined boundary,
   with resultant reduction in both hodograph size and low-level
   convergence.

   ..Edwards.. 02/26/2018

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