SPC AC 060410
Day 2 Convective Outlook
NWS Storm Prediction Center Norman OK
1010 PM CST Sat Feb 05 2022
Valid 071200Z - 081200Z
...NO THUNDERSTORM AREAS FORECAST...
...SUMMARY...
The risk for thunderstorms appears negligible across the U.S.,
Monday through Monday night.
...Discussion...
Based on the latest deterministic and ensemble output of the various
models, it still appears likely that a blocking mid-level high will
become more prominent once again, to the west of the U.S. Pacific
coast during this period. This is forecast to occur as a fairly
significant short wave trough continues inland, around the periphery
of persistent larger-scale ridging within the mid-latitude
westerlies across the eastern Pacific into western North America.
As the ridging rebuilds to the north of the center of the developing
high, the downstream short wave trough appears likely to dig to the
lee of the Canadian and northern U.S. Rockies, across the Canadian
Prairies and adjacent international border area.
There is at least somewhat greater spread concerning short wave
developments within splitting downstream stream flow, from the Great
Plains and Mexican Plateau eastward through the Atlantic Seaboard.
However, even as initially deep eastern Canadian mid-level troughing
retreats to the higher latitudes, mid-level flow across the central
into eastern U.S. will remain broadly confluent, to the northwest of
somewhat more amplified southwestern Atlantic subtropical ridging.
It does still appear that forcing for ascent, downstream of
mid-level short wave troughing within this regime, may support
continued weak to modest surface cyclogenesis along a frontal zone
off the southern Mid Atlantic coast Monday through Monday night.
However, destabilization supportive of an appreciable risk for
thunderstorms probably will remain confined to areas near and east
of the Gulf Stream.
Otherwise, the boundary-layer over much of the northern and western
Gulf Basin is forecast to remain relatively cool and stable. Ahead
of lingering mid-level troughing across the Mexican Plateau, it
still appears that elevated moisture return of subtropical eastern
Pacific origin, coupled with some steepening of mid-level lapse
rates, may be contributing to weak conditional and convective
instability (based near or above 700 mb) across parts of the lower
Rio Grande Valley at the outset of the period. However, the
potential for this to support convection capable of producing
lightning remains unclear, but seems rather low at best.
..Kerr.. 02/06/2022
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