Day 2 Convective Outlook
NWS Storm Prediction Center Norman OK
1254 AM CST Fri Dec 31 2021
Valid 011200Z - 021200Z
...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS ACROSS PORTIONS
OF THE DEEP SOUTH AND TENNESSEE VALLEY....
...SUMMARY...
Widespread thunderstorms are expected from the ArkLaTex to the
Western Appalachians on New Year's Day. All severe-weather hazards
are possible including large hail, damaging winds, and tornadoes, a
couple of which may be strong.
...Synopsis...
A positively tilted upper-level trough will be centered near the
Great Basin to start the period. This trough will maintain its
positive tilt as it shifts eastward across the Plains and into the
Midwest by 12Z Sunday. An embedded mid-level shortwave trough will
move quickly from the southern High Plains across the Midwest and
Ohio Valley Saturday to the Northeast by Sunday morning. A surface
reflection of this mid-level shortwave trough is expected to travel
along the front from the Ozarks to the Ohio Valley and into the
Mid-Atlantic.
...Ohio Valley into the central Appalachians...
There is still considerable uncertainty regarding the northward
extent of the destabilization and severe-weather threat based on the
position of the position of the surface front and the strength of
the surface low. The NAM is stronger with the surface low with a
much farther north warm front bringing low 60s dewpoints north of
the Ohio River into southern Illinois, southern Indiana, and
Southwest Ohio. However, the operational GFS is much weaker and
southeast with the surface low and only brings low 60s dewpoints
into south-central Kentucky. The ECMWF solution is between these two
locations with the frontal position, which also closely resembles
the GEFS mean. Therefore, the northern extent of the marginal and
slight risk threat areas match the ECMWF and GEFS mean.
A line of storms is expected to move through this region during the
afternoon and early evening hours. Forecast soundings show more than
50 knots of flow only a few hundred meters above the surface.
Therefore, mixing this strong flow to the surface should not be that
difficult, even in a weak buoyancy environment. Low 60s dewpoints
should yield MLCAPE around 250 to 500 J/kg across southern Kentucky,
which increases the confidence for severe winds as the squall line
moves through. In addition, a QLCS tornado threat will exist given
the strong low-level speed shear present ahead of this line of
storms. However, the limited instability and veered surface flow
will be limiting factors to a greater tornado threat along this
portion of the line.
...Portions of the Deep South into the Tennessee Valley...
A large area of thunderstorms, some of which may be severe, is
expected to be ongoing from western Kentucky to northern Texas
Saturday morning. As the surface low moves from the Plains into the
Ozarks Saturday morning, this convection is expected to become
better organized, likely into a squall line, and start to advance
eastward. Dewpoints are forecast in the mid to upper 60s ahead of
these storms, which should yield MLCAPE around 500 to 1500 J/kg from
north to south. This should be more than sufficient to maintain a
strong squall line through the afternoon and into the overnight
hours across eastern Arkansas, most of Tennessee, and northern
Mississippi and Alabama. A 50 to 60 knot low-level jet will result
in strong low-level speed shear across the entire warm sector.
Forecast soundings show mostly unidirectional flow in the lowest 1
km due to the veered surface flow across most of the warm sector as
a result of the elongated nature of the surface pressure pattern.
This should temper the tornado threat somewhat, but with the strong
speed shear and the expectation of a well balanced squall line, the
environment will still be supportive for QLCS tornadoes.
Most guidance hints at the potential for some warm sector supercell
development across portions of Mississippi, Alabama, and Tennessee
Saturday afternoon/evening. The ECMWF has been especially bullish
with pre-frontal convection for the last several days, which
continues through the latest 00Z run. Any strong supercells which
can develop in the open warm sector will likely have the greatest
threat for significant to potentially intense tornadoes. The most
likely region for pre-frontal supercell development will be from
eastern Arkansas to northern Alabama and possibly southern Tennessee
where greater instability is forecast. Veered low-level flow will
keep low-level directional shear limited during the first half of
the day. However, at least slightly greater low-level turning is
shown by forecast soundings during the late afternoon into the
evening hours as surface flow remains south-southwest, while the
low-level jet starts to veer more westerly as the main wave shifts
east. This may result in a slightly higher tornado threat into the
overnight hours from far eastern Mississippi into northern/central
Alabama and northwest Georgia.
..Bentley.. 12/31/2021
Nothing says Happy New Year than a large 10% hatched tor prob
Day 2 Convective Outlook NWS Storm Prediction Center Norman OK 1254 AM CST Fri Dec 31 2021 Valid 011200Z - 021200Z ...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS ACROSS PORTIONS OF THE DEEP SOUTH AND TENNESSEE VALLEY.... ...SUMMARY... Widespread thunderstorms are expected from the ArkLaTex to the Western Appalachians on New Year's Day. All severe-weather hazards are possible including large hail, damaging winds, and tornadoes, a couple of which may be strong. ...Synopsis... A positively tilted upper-level trough will be centered near the Great Basin to start the period. This trough will maintain its positive tilt as it shifts eastward across the Plains and into the Midwest by 12Z Sunday. An embedded mid-level shortwave trough will move quickly from the southern High Plains across the Midwest and Ohio Valley Saturday to the Northeast by Sunday morning. A surface reflection of this mid-level shortwave trough is expected to travel along the front from the Ozarks to the Ohio Valley and into the Mid-Atlantic. ...Ohio Valley into the central Appalachians... There is still considerable uncertainty regarding the northward extent of the destabilization and severe-weather threat based on the position of the position of the surface front and the strength of the surface low. The NAM is stronger with the surface low with a much farther north warm front bringing low 60s dewpoints north of the Ohio River into southern Illinois, southern Indiana, and Southwest Ohio. However, the operational GFS is much weaker and southeast with the surface low and only brings low 60s dewpoints into south-central Kentucky. The ECMWF solution is between these two locations with the frontal position, which also closely resembles the GEFS mean. Therefore, the northern extent of the marginal and slight risk threat areas match the ECMWF and GEFS mean. A line of storms is expected to move through this region during the afternoon and early evening hours. Forecast soundings show more than 50 knots of flow only a few hundred meters above the surface. Therefore, mixing this strong flow to the surface should not be that difficult, even in a weak buoyancy environment. Low 60s dewpoints should yield MLCAPE around 250 to 500 J/kg across southern Kentucky, which increases the confidence for severe winds as the squall line moves through. In addition, a QLCS tornado threat will exist given the strong low-level speed shear present ahead of this line of storms. However, the limited instability and veered surface flow will be limiting factors to a greater tornado threat along this portion of the line. ...Portions of the Deep South into the Tennessee Valley... A large area of thunderstorms, some of which may be severe, is expected to be ongoing from western Kentucky to northern Texas Saturday morning. As the surface low moves from the Plains into the Ozarks Saturday morning, this convection is expected to become better organized, likely into a squall line, and start to advance eastward. Dewpoints are forecast in the mid to upper 60s ahead of these storms, which should yield MLCAPE around 500 to 1500 J/kg from north to south. This should be more than sufficient to maintain a strong squall line through the afternoon and into the overnight hours across eastern Arkansas, most of Tennessee, and northern Mississippi and Alabama. A 50 to 60 knot low-level jet will result in strong low-level speed shear across the entire warm sector. Forecast soundings show mostly unidirectional flow in the lowest 1 km due to the veered surface flow across most of the warm sector as a result of the elongated nature of the surface pressure pattern. This should temper the tornado threat somewhat, but with the strong speed shear and the expectation of a well balanced squall line, the environment will still be supportive for QLCS tornadoes. Most guidance hints at the potential for some warm sector supercell development across portions of Mississippi, Alabama, and Tennessee Saturday afternoon/evening. The ECMWF has been especially bullish with pre-frontal convection for the last several days, which continues through the latest 00Z run. Any strong supercells which can develop in the open warm sector will likely have the greatest threat for significant to potentially intense tornadoes. The most likely region for pre-frontal supercell development will be from eastern Arkansas to northern Alabama and possibly southern Tennessee where greater instability is forecast. Veered low-level flow will keep low-level directional shear limited during the first half of the day. However, at least slightly greater low-level turning is shown by forecast soundings during the late afternoon into the evening hours as surface flow remains south-southwest, while the low-level jet starts to veer more westerly as the main wave shifts east. This may result in a slightly higher tornado threat into the overnight hours from far eastern Mississippi into northern/central Alabama and northwest Georgia. ..Bentley.. 12/31/2021 Nothing says Happy New Year than a large 10% hatched tor prob
