10/14/2017
Day 2 Convective Outlook
NWS Storm Prediction Center Norman OK
1156 AM CDT Sat Oct 14 2017
Valid 151200Z - 161200Z
...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS OVER THE LOWER
GREAT LAKES REGION....
...SUMMARY...
Showers and a few thunderstorms producing strong to locally damaging
wind gusts will be possible across parts of the lower Great Lakes
region Sunday afternoon.
...Synopsis...
A progressive upper flow pattern is forecast to continue tomorrow as
a vigorous upper trough currently over the central Rockies
accelerates across the Great Lakes and southeast Canada. At the
surface, a low is expected to deepen as it moves from the Great
Lakes toward southern Quebec, with a strong trailing cold front
moving rapidly eastward across the northeastern states during the
period.
...Lower Great Lakes Region...
A moist air mass will be in place in the warm sector tomorrow with
surface dew points in the 60s. However, thermodynamic profiles
appear marginal for thunderstorm development as meager lapse rates
and relatively warm mid-level temperatures limit instability, with
SBCAPE generally less than 500-750 J/kg. Despite the weak
thermodynamic environment, very strong isallobaric forcing along the
cold front will coincide with the right entrance region of a strong
upper level jet core advancing from the lower Great Lakes into the
St. Lawrence Valley. This will support development of a narrow,
low-topped QLCS along the cold front, consistent with guidance from
numerous 12Z CAMs and HREFv2 guidance.
Strong winds aloft will be located near the cold front with 50-60 kt
at 850 mb, and forecast soundings show stronger low-level winds
lowering to near the surface along and immediately behind the cold
front. This process will be potentially aided by convective
downdrafts within the QLCS vertical circulation, suggesting a threat
for strong to locally damaging winds as the narrow convective line
moves rapidly eastward during the afternoon. The
convectively-enhanced wind threat should gradually diminish by
evening with the onset of boundary layer cooling and stabilization.