Wednesday, March 1, 2017

SPC Mar 1, 2017 2000 UTC Day 1 Convective Outlook

SPC 2000Z Day 1 Outlook
Day 1 Outlook Image
Day 1 Convective Outlook  
NWS Storm Prediction Center Norman OK
0218 PM CST Wed Mar 01 2017

Valid 012000Z - 021200Z

...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS EXTENDING FROM
PORTIONS OF EAST-CENTRAL MISSISSIPPI...NORTHERN ALABAMA...NORTHERN
GEORGIA...AND FAR EASTERN TENNESSEE TO COASTAL AREAS OF THE
MID-ATLANTIC STATES...

...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS SURROUNDING THE
ENHANCED RISK FROM THE CENTRAL GULF COAST STATES TO SOUTHERN NEW
ENGLAND...

...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS EXTENDING FROM
THE CENTRAL GULF COAST STATES TO THE UPPER OHIO VALLEY AND SOUTHERN
NEW ENGLAND...

...SUMMARY...
Severe thunderstorms with damaging winds are expected from portions
of the Southeast to the Mid Atlantic region and parts of southern
New England. Damaging winds will be likely, and the risk for
tornadoes will exist particularly from parts of east-central
Mississippi to portions of north Georgia and vicinity.

...Southern New England to the Mid-Atlantic States...
Severe weather threat remains valid for southern New England toward
DelMarVA as the environment destabilizes poleward, with surface dew
points in the 60s now spreading north across NJ.  The western parts
of Mid-Atlantic severe probabilities have been trimmed from the
convective outlook, as the air mass has stabilized in the wake of
the storms now reaching parts of the East Coast States.  A marginal
risk remains for isolated strong to possibly severe storms across
the upper OH Valley into western PA as discussed in the previous
outlook.

Residual moisture located across southern VA in vicinity of the
trailing portion of a convective outflow boundary extending
southwest from southeast VA to far northwest NC may depict the
northern extent of a severe-weather threat as strong to severe
storms spread east from the southern Appalachians.  The downstream
air mass across the Carolinas will continue to destabilize with
strong deep-layer and low-level shear supporting all severe hazards
into this evening.

...Carolinas/Southeast States to lower MS Valley...
Strong to severe storms will continue to develop along and ahead of
the cold front as it advances through this region of the U.S. during
the remainder of the afternoon and through the evening and early
overnight.  Previous forecast reasoning remains valid, while the
western portions of this outlook have been trimmed with the passage
of the ongoing band of storms extending from LA to middle and
eastern TN as the environment stabilizes in the wake of this
activity.

..Peters.. 03/01/2017

.PREV DISCUSSION... /ISSUED 1028 AM CST Wed Mar 01 2017/

...Portions of the Southeast to the Mid-Atlantic region and southern
New England...

An extensive belt of strong mid/high-level flow across the Southern
and Eastern States will maintain strong deep shear over a moist and
diurnally destabilizing warm sector across the area. A squall line
from Middle TN toward the central Appalachians will likely spread
across the adjacent Piedmont during the next several hours.
Re-intensification of this activity is expected, owing to the
presence of adequate moisture return (upper 50s to lower 60s
dewpoints) amidst surface heating and relatively steep midlevel
lapse rates. Swaths of damaging wind gusts will be likely as this
activity spreads toward the coastal plain through the evening. A
couple of tornadoes will be possible. Severe-wind probabilities have
been increased eastward across the Piedmont area.

More separated updrafts/discrete convection are evolving across
parts of the lower MS Valley, at the southern end of a zone of
stronger deep ascent. As this activity spreads eastward toward parts
of the southern Appalachians and vicinity, it will intercept a
relatively more moist boundary layer supporting stronger instability
further aided by steep midlevel lapse rates (around 8.5 C/km in the
700-500-mb layer per the 12Z Jackson sounding). With 250-350 m2/s2
of effective SRH associated with modestly curved though long
hodographs, tornado probabilities have been increased in this area.

With northward extent across the East (i.e., toward southern New
England and vicinity), weaker instability will exist owing to more
widespread cloud coverage amidst an antecedent cooler/drier boundary
layer. However, strong vertical shear profiles will support a
conditional severe risk.

Modest destabilization may take place around the upper Ohio Valley
and eastern Great Lakes area amidst recycled moisture ahead of the
primary cold front, perhaps supporting a band of strongly forced
convection spreading eastward from the late afternoon through the
evening. Locally damaging wind gusts may accompany this activity.

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