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ACUS01 KWNS 141302
SWODY1
SPC AC 141301
Day 1 Convective Outlook CORR 1
NWS Storm Prediction Center Norman OK
0801 AM CDT Mon May 14 2018
Valid 141300Z - 151200Z
...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS FROM PARTS OF
OHIO SOUTHEASTWARD TO THE EASTERN VIRGINIA/SOUTHERN MARYLAND
TIDEWATER REGION...
CORRECTED FOR TWO HAIL POINTS
...SUMMARY...
Damaging thunderstorm wind appear probable from parts of Ohio to the
mid/lower Chesapeake Bay region. Other thunderstorms, capable of
isolated damaging wind and large hail, are expected from parts of
the southern Plains to the Ohio Valley.
...Synopsis...
In mid/upper levels, a split-flow regime will persist through the
period across the West, with downstream cyclonic flow over the Great
Lakes and upper Midwest. A temporary Rex pattern will develop over
the Great Basin and Northwest as a 500-mb high moves eastward over
WA/northern ID, while the long-lasting, quasistationary cyclone
centered over northern NV continues to slowly weaken and drift
erratically near its present position. Upper ridging -- now evident
in moisture-channel imagery from MO to the Dakotas -- is forecast to
flatten through the period as heights gradually fall over the Great
Lakes, and a series of low-amplitude perturbations crosses the
Plains and Midwest through the current ridge position. Meanwhile, a
broad deep-layer cyclone -- centered initially over the northeastern
gulf southwest of TBW, is progged to meander irregularly northward
toward the FL Panhandle through the period.
At the surface, a wavy/quasistationary frontal zone was analyzed at
11Z from near the mouth of Chesapeake Bay northwestward across
north-central VA to west-central/southwestern OH, then westward to
the MO/IA border region and a weak frontal-wave low near FNB. The
front extended southwestward to another weak low in the DHT-CAO
region. A dryline extended from there southward into the Big Bend
region of TX. As the dryline mixes eastward across the Panhandles,
South Plains and Permian Basin today, the low will shift eastward
along the triple point. The remainder of the frontal zone will be quasistationary, except where modulated my mesoscale convective
processes. An arctic cold front -- related to a strong mid/upper
cyclone forecast to cross Hudson Bay through the period -- will move southeastward from northern ON across parts of the upper Great Lakes
region overnight.
...Ohio Valley to VA/MD Tidewater...
Potential is increasing for a relative concentration of northwest-southeast-moving thunderstorms today, the primary hazard
being damaging wind. An ongoing/elevated and non-severe
thunderstorm complex has been occurring for a few hours north of the
frontal zone, across portions of the southern Lake Michigan vicinity
eastward over southern Lower MI, northern IN and northwestern OH.
Most of this activity should remain north of the boundary and weaken
with time this morning as the LLJ supplying its predominant inflow
layer weakens. However, surface isallobaric analysis shows a
corridor of pressure rises 2-3 mb per 2 hours penetrating the stable
layer poleward of the front, an indicator of reasonably substantial, convectively induced/aided perturbation in the low levels.
As the related UVV field approaches the diabatically destabilizing
warm sector and frontal surface convergence/vorticity max later this
morning over OH, additional/organized convective development and
subsequent upscale growth are becoming increasingly probable. The
foregoing preconvective/warm-sector environment across parts of
OH/WV will be characterized in lower elevations by surface dew
points 60s F, underlying 700-500-mb lapse rates 7.5-8.5 deg C/km.
While the lapse rates will diminish with southeastward extent, the
air mass will remain favorably unstable/buoyant to support damaging-wind-producing thunderstorms riding the frontal
baroclinic/instability gradient, potentially all the way to the
Chesapeake Bay region. Width/depth of any cold-pool development
within such a complex remains uncertain; however, the increasing
potential for such upscale organization warrants a relatively
enhanced corridor of wind probabilities within the much lengthier
15%/slight area at this time.
...Southern Plains to Midwest...
Scattered to numerous thunderstorms in clusters are expected to
develop along the dryline and frontal zone, offering large hail and strong-severe gusts as they move eastward to southeastward. Some of
this activity may aggregate into larger/forward-propagational
multicellular complexes, with the severe threat transitioning from a
hail/wind blend to more purely wind. While relative concentrations
of hail (in western areas) and wind at 30%+ unconditional levels
probably will occur somewhere within this corridor, many of the
factors contributing to such evolution would develop from mesobeta-
to storm-scale processes that remain uncertain, undeveloped and
non-specific at this time. As such, will maintain the general
slight-risk area for now, acknowledging the potential for a node or
two of enhanced risk to become apparent within.
Elevated mixed-layer air has overspread this region for several
days, yielding a plume of steep midlevel lapse rates. However,
planar analyses and cross-sections in the 850-500-mb layer indicate
the basal capping layer of the EML should not be as strong for
preconvective MLCINH as in previous days. A swath of preconvective
MLCAPE 3500-4500 J/kg is expected to develop over much of OK, with
values at least briefly exceeding 3000 J/kg elsewhere from
central/western MO to the Rio Grande Valley of southwest TX.
1500-2000 J/kg values are possible farther east and northeast across
the Corn Belt, associated with somewhat weaker CINH and smaller
lapse rates characterizing less-pristine EML trajectories.
Given these factors, development in general may occur somewhat
sooner in the diabatic-heating cycle, and become more dense in
ultimate concentration, with greater longevity and farther downshear
spread before weakening. Weak low/middle-level flow and lack of
more robust vertical shear should contribute to predominant
multicellular organization. A combination of spreading outflow and
diabatic cooling of the moist sector's boundary layer will adversely
reduce available instability tonight and lead to general weakening.
...Eastern CO and vicinity...
Widely scattered to scattered thunderstorms should develop this
afternoon over the higher terrain of the eastern mountains/
foothills, where diabatic heating and orographic lift will weaken
MLCINH fastest. Activity should pose a risk if isolated severe
hail/gusts as it moves into the adjoining High Plains, and a tornado
cannot be ruled out. Forecast soundings suggest sufficient
near-surface moistening and diabatic destabilization to support
500-1000 J/kg MLCAPE. Easterly boundary-layer flow components
northwest of the surface low will support strong-severe convective
potential over this area via upslope lift, moisture advection/
transport, relatively maximized storm-relative low-level flow, and
vector augmentation of deep shear. Although low-level flow will be
weak -- limiting hodograph size and magnitude of low-level bulk
shear -- strong directional shear and the potential for storm-scale/
boundary interactions indicates potential for at least short-lived
supercell mode, with non-negligible tornado potential.
...Southeast/east-central FL...
Surface data and available RAOBs/VWP indicate a narrow corridor of
favorable conditions for short-lived supercells and threat for a
brief tornado or two from any sustained convection, for at least
another few hours. This potential is related to a coast-parallel
onshore convergence zone located just inland that may shift northward/northwestward through the remainder of the morning. West
of that boundary, backed flow maximizes effective SRH, and east of
it resides a relatively undisturbed Gulf Stream air mass maximizing
theta-e and CAPE. The scenario loosely resembles a buoyancy/shear
overlap archetype in marginal tropical cyclones, with more
localized/transient risk, given the weaker ambient flow
characterizing this nontropical system. See NHC forecast
discussions for more information on potential for eventual
subtropical or tropical development with the Gulf low.
..Edwards/Mosier.. 05/14/2018
$$
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