000
FXUS64 KFWD 040102
AFDFWD
Area Forecast Discussion
National Weather Service Fort Worth TX
802 PM CDT Sun Apr 3 2022
...New Short Term, Aviation...
.SHORT TERM... /NEW/
/Through Monday Night/
Bottom Line:
Rain and
thunderstorm chances begin increasing across North and
Central Texas this evening/tonight with the potential for a few
strong storms capable of producing small
hail and strong wind
gusts in our northwestern zones. The threat for strong and severe
thunderstorms will increase late Monday afternoon through Monday
night region-wide. All hazards including large
hail, damaging
winds, and a few tornadoes are possible Monday. Additionally,
heavy
rainfall may result in localized urban and small stream
flooding despite ongoing
drought conditions.
Meteorological Analysis:
In response to the modest southerly breeze in place this
afternoon, the poleward transport of Gulf
moisture has served to
sharpen a diffuse western north-central Texas surface dryline,
extending from Quanah, TX southwestward towards Midland, TX. The
warm sector is further outlined by a
quasi-stationary cold
front,
associated with a northern stream
shortwave trough advancing
across the Northern Plains. Surface analysis showed the cold
front
draped from near Topeka in northeastern KS, to Cherokee in
northwestern OK, to Childress in the southern TX panhandle.
Regional radars indicate the initiation of
convection in a fairly
narrow corridor just ahead of the dryline. In this region,
synoptic-scale ascent associated with the
deepening upper
trough
to our west is arriving while localized lift focused along the
dryline/cold
front, low-level warm
advection/surface heating, and
a strengthening low-level
jet which is sending a deep
surge of
moisture east of the dryline is supporting
thunderstorm
development.
Latest high-resolution model guidance suggests that
instability
is locally confined along and just ahead of the dryline with a
semi-discrete/discrete supercellular convective mode favored due
to increasing effective
shear and the orientation of mid-level
flow in relation to the surface boundary. This activity is
progged
to move eastward through the late evening, crossing our
northwestern/western zones overnight. As the
convection becomes
further displaced from the boundary, the environment will become
less supportive of severe weather, however a few thunderstorms may
still be strong enough to carry a threat for small
hail and gusty
downdraft winds. Even the most aggressive CAMs do not maintain
convection to the Interstate 35 corridor so it is
likely that most
of North Texas will remain dry tonight. Low
PoPs have been
maintained across parts of North Texas through daybreak Monday as
additional showers and sub-severe thunderstorms may develop in the
vicinity of residual
outflow boundaries from decaying
convection.
By Monday morning, the stalled
front will have settled over
south-central Oklahoma and far western North Texas. Convective
activity through the morning hours should remain anchored near
this boundary though there is the potential for a few shallow warm
advection showers to develop across North and Central Texas as
low-level
flow continues to transport
moisture into the region
(dewpoints near 60 degrees approaching the Red River). Most areas
are
likely to remain dry throughout much of the day however due to
the absence of forcing in the lower levels and the delayed
erosion of the
EML/MLCIN. Though cloud cover will generally
inhibit
diurnal heating, ongoing
WAA and steepening mid-level
lapse rates ahead of the approaching upper
trough will lead to
eventual destabilization as the nearly stationary
front north of
the region begins to be pulled south/southeast into our western
zones.
Convective intensity and coverage is expected to increase Monday
evening and into the overnight hours as surface-based
thunderstorms erupt near the
front/dryline. Vertical
veering of
wind profiles with
height should favor discrete supercells
initially, with the highest potential further south in
southwestern Central Texas along the dryline with large
hail,
damaging wind gusts, and a
tornado or two possible. Upscale
development into larger clusters and eventually an eastward-
advancing QLCS continues to be the most probable evolution as
storms will
likely struggle to remain discrete amid the
increasing low-level
jet and deep-layer
flow parallel to portions
of the surface boundary. The CAMs have favored this evolution for
several runs even as
mesoscale details have wavered. This
convective activity will progressively march across most of North
and Central Texas before midnight. While the
tornado and large
hail threat will be higher with any storms that manage to remain
discrete, the environment is still
likely to be supportive of all
severe weather hazards including areas of widespread damaging
winds and a few embedded QLCS tornadoes given the strong low level
shear in place. The general timing for the peak severe weather
threat across our forecast area will be 7 PM CDT Monday to 12 AM
CDT Tuesday, so it is very important for everyone to have multiple
methods of receiving warnings through the overnight hours. In
addition to the severe weather threat, locally high rain rates may
result in
isolated minor flooding, especially in low-lying and
flood prone areas, despite the anticipated progressive pace of
convection.