Tuesday, October 30, 2018

Oct 30, 2018 1300 UTC Day 1 Convective Outlook - Ciela Marie Acala

Day 1 Convective Outlook  
   NWS Storm Prediction Center Norman OK
   0755 AM CDT Tue Oct 30 2018

   Valid 301300Z - 311200Z

   ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS OVER PARTS OF
   WEST-CENTRAL TEXAS LATE OVERNIGHT...

   ...SUMMARY...
   Thunderstorms late overnight into the predawn hours Wednesday may
   produce severe hail over parts of west Texas.

   ...Synopsis...
   In mid/upper levels, a progressive pattern will prevail over the
   forecast area.  The most important synoptic feature is a broad area
   of cyclonic flow and related troughing now over the western U.S.,
   extending southwestward from a cyclone over the MB/SK border to the
   lower Colorado River Valley.  Several initially lower-amplitude,
   embedded shortwave perturbations now across the Pacific Northwest
   and Great Basin will phase into a more coherent, strong, basal
   shortwave trough by 12Z from the Four Corners region across southern
   AZ and northern Sonora.  Meanwhile the Canadian cyclone will
   progress to far northwestern ON near the MB border, its shortwave
   trough extending southward then southwestward over the Upper
   Mississippi Valley region.  A broad fetch of low-/middle-level
   southwesterlies and related low-level warm-advection regime will
   spread across much of the mid-Mississippi and Ohio Valleys and
   vicinity.

   At the surface, 11Z analysis showed a low over southern MN, with
   cold front southwestward across west-central IA, northeastern to
   south-central KS, central TX Panhandle, and northeastern NM.  By
   00Z, the low should weaken somewhat as it reaches northern Lake
   Michigan, with cold front southwestward over northern IL,
   southwestern MO, south-central OK, west-central TX, and southeastern
   NM.  By 12Z, the front should reach northwestern OH, southern IL,
   the AR Ozarks, north-central TX, and the Edwards Plateau. 

   ...West-central TX late overnight...
   Widely scattered to scattered thunderstorms are forecast to develop
   behind the surface cold front, during the last few hours of the
   period, over parts of the Permian Basin region into west-central TX.
    As this activity moves eastward to northeastward toward the Big
   Country and Concho Valley regions, it will encounter increasingly
   high-theta-e low-level trajectories atop the frontal surface. 
   Related low-level warm advection will contribute to steepening
   midlevel lapse rates ahead of the amplifying Four Corners
   perturbation, resulting in increasing elevated buoyancy, amidst
   strengthening deep shear.  By the 09-12Z time frame, forecast
   soundings yield MUCAPE in the 1500-2000 J/kg range, collocated with
   45-60 kt effective-shear vectors.  To the extent storm modes can
   stay relatively clean and discrete long enough, large hail will be a
   concern.  At this time, that modal conditionality precludes more
   than a marginal hail outlook, but at least isolated severe hail now
   appears probable over the region during the predawn hours. 

   ...Eastern IA/northern IL/southern WI region this afternoon...
   Low-level warm advection and modest, early-stage moisture return
   will support isolated to scattered convective development near the
   front this afternoon into evening, from the IA/WI/IL area to eastern
   OK, potentially backbuilding into parts of north TX tonight.  The
   largely front-parallel nature of flow aloft, anafrontal character of
   the progressive boundary with respect to convective development, and
   lack of more robust moisture should limit the potential for
   organized severe overall in this regime day-1.  

   Strong thunderstorms with isolated, mainly subsevere hail may occur
   this afternoon from eastern IA across the WI/IL border region, as
   the low-level frontal zone and some weak large-scale ascent from a
   northern-stream perturbation encounter the northwestern rim of the
   elevated warm-advection/moisture-transport belt.  Forecast soundings
   suggest the potential for up to about 1200 J/kg of elevated MUCAPE
   to develop in the most aggressive moistening scenarios above the
   stable boundary layer.  Convection-allowing guidance reasonably
   indicates a rather messy, streaky, clustered mode in this regime,
   which in tandem with limited inflow-layer moisture content, would
   tend to temper duration and size of hail.  At this time the risk
   appears too uncertain for an unconditional marginal-severe area.

   ..Edwards/Peters.. 10/30/2018



https://www.spc.noaa.gov/products/outlook/day1otlk.html


posted by: Ciela Marie Acala

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