...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS TUESDAY EVENING
INTO TUESDAY NIGHT ACROSS SOUTHEASTERN LOUISIANA AND
MISSISSIPPI...SOUTHWESTERN ALABAMA AND THE WESTERN FLORIDA
PANHANDLE...
...SUMMARY...
Severe thunderstorms are possible near mid to upper Texas coastal
areas Tuesday afternoon, before spreading into parts of southeastern
Louisiana and Mississippi through southwestern Alabama and the
western Florida Panhandle Tuesday night. These storms will be
accompanied by a risk for potentially damaging wind gusts and
tornadoes, a few of which could be strong.
...Synopsis...
An initially prominent mid-level high over the southern mid-latitude
Pacific likely will weaken, with a new high center gradually
beginning to form in higher latitudes, within persistent
larger-scale ridging. This ridging is forecast to continue to build
north-northeastward across British Columbia, Yukon and parts of the
Northwest Territories Tuesday through Tuesday night, with amplified
large-scale troughing being maintained downstream, along and east of
the Rockies Mountains. The most prominent perturbation within this
regime, initially a vigorous short wave trough with a compact,
embedded deep mid-level low, is still forecast to accelerate out of
the base of the troughing by early Tuesday.
The NCEP SREF remains notably slower than most other model output,
which generally indicates that the perturbation will rapidly
progress across the southern Great Plains into the Mid South by late
Tuesday night, accompanied by significant surface cyclogenesis near
mid/upper Texas coastal areas into the lower Mississippi Valley,
then north-northeastward into the Mid South. As this occurs, an
intense west-southwesterly mid/upper jet (including 90-100 kt around
500 mb) is forecast to develop across the lower Mississippi through
Tennessee Valleys by 12Z Wednesday. In association with the
developing cyclone, a southerly low-level jet may include speeds
increasing to 50-70 kt, and perhaps even stronger to the east of the
lower Mississippi Valley during a period of more rapid deepening
Tuesday evening.
...Southeast Texas coastal through central Gulf Coast states...
With little appreciable change to model forecasts concerning the
synoptic forcing, the presence of an initially cool/stable
boundary layer across much of the Gulf Coast region remains the
primary potential limiting factor to the development of a more
substantive risk for severe thunderstorms Tuesday through Tuesday
night. The boundary layer across much of the northern Gulf of
Mexico will also still be in the process of modifying from prior
frontal intrusions, but it does appear that mid/upper 60s F surface
dew points will rapidly advect toward northwestern through north
central Gulf coastal areas, and perhaps at least a bit inland.
Near-surface destabilization across and inland of mid into
upper Texas coastal areas will contribute to an environment
conducive to organizing convective development, including supercells
Tuesday afternoon. Thereafter, similar destabilization in a
corridor across southeastern Louisiana into southwestern
Alabama still seems probable Tuesday evening through Tuesday night.
Beneath a plume of modestly steepening lapse rates, this is expected
to contribute to a corridor of destabilization sufficient to
maintain an organized convective cluster or line, with embedded
supercells, along an eastward advancing pre-cold frontal confluence
zone. Aided by low-level warm advection in advance of this
activity, this may be preceded by a few discrete supercells.
It is still possible that a residual layer of moist adiabatic to
more stable near-surface lapse rates within the warm sector could
tend to minimize the number of potentially severe storms. However,
the latest (23/03Z) forecast soundings from the Rapid Refresh, which
extend out through 06Z Tuesday night, increase confidence for at
least weak surface-based destabilization to occur in a corridor
across southeastern Louisiana into southwestern Alabama/western
Florida Panhandle. With low-level hodographs forecast to become
very large and clockwise curved, in the presence of strong
deep-layer shear, the environment may become supportive of a couple
strong tornadoes in the supercell storms.