Jan 1, 2018 0830 UTC Day 3 Severe Thunderstorm Outlook
Updated: Mon Jan 1 06:00:04 UTC 2018 (20180101 0830Z Day 3 shapefile | 20180101 0830Z Day 3 KML)
Probabilistic to Categorical Outlook Conversion Table
Categorical Graphic
20180101 0830 UTC Day 3 Outlook Graphic
Day 3 Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
No Risk Areas Forecast
Probabilistic Graphic
20180101 0830 UTC Day Probabilitic Graphic
Probability of severe weather within 25 miles of a point.
Hatched Area: 10% or greater probability of significant severe within 25 miles of a point.
Day 3 Prob. Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
No Risk Areas Forecast
   SPC AC 010600

   Day 3 Convective Outlook  
   NWS Storm Prediction Center Norman OK
   1200 AM CST Mon Jan 01 2018

   Valid 031200Z - 041200Z

   ...NO SEVERE THUNDERSTORM AREAS FORECAST...

   ...SUMMARY...
   Some thunderstorm activity is possible near central California
   coastal areas late Wednesday afternoon and evening, but the risk for
   severe storms appears negligible.

   ...Discussion...
   Mid/upper flow will remain amplified across North America through
   this period.  In association with one significant short wave within
   larger-scale troughing across the East, models continue to indicate
   that strong cyclogenesis will take place over the western Atlantic,
   near/north of the Bahamas northeastward toward the Canadian
   Maritimes.  In the wake of this feature, generally cold and stable
   conditions likely will continue across most areas east of the
   Rockies.

   Meanwhile, large-scale ridging, within perhaps a couple of
   increasingly in-phase belts of westerlies, is expected to persist
   across much of western North America.  However, it does appear that
   the remnants of a southern stream closed low may accelerate
   north/northeastward into portions of central and northern California
   late Wednesday into Wednesday night.  While the mid-level cold pool
   with this feature may not be particularly cold (warmer than -20C),
   models suggest that an influx of moisture from the lower latitudes
   could perhaps still contribute to mid-level destabilization
   supportive of convection capable of producing lightning, into at
   least the vicinity of central California coastal areas.

   ..Kerr.. 01/01/2018

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