Sep 2, 2017 1730 UTC Day 2 Convective Outlook
Updated: Sat Sep 2 17:29:35 UTC 2017 (20170902 1730Z Day 2 shapefile | 20170902 1730Z Day 2 KML)
Probabilistic to Categorical Outlook Conversion Table
Categorical Graphic
20170902 1730 UTC Day 2 Outlook Graphic
Day 2 Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
No Risk Areas Forecast
Probabilistic Graphic
20170902 1730 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 2 Prob. Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
No Risk Areas Forecast
   SPC AC 021729

   Day 2 Convective Outlook  
   NWS Storm Prediction Center Norman OK
   1229 PM CDT Sat Sep 02 2017

   Valid 031200Z - 041200Z

   ...NO SEVERE THUNDERSTORM AREAS FORECAST...

   ...SUMMARY...
   The risk of severe thunderstorms appears negligible (i.e., severe
   probabilities less than 5 percent) across the U.S., Sunday through
   Sunday night.

   ...Synopsis...
   Subtropical ridging appears likely to remain prominent across much
   of the West through this period, generally centered along an axis
   extending from the Cascades through the southern Rockies.  On its
   southwestern periphery, a weakening tropical cyclone (Lidia) is
   forecast to progress slowly northwest of Baja.  This probably will
   be accompanied by an influx of seasonably high moisture content air
   into at least portions of the southwestern deserts and southern
   California.

   To the north, models suggest that the mid-latitude westerlies may
   become increasing amplified across the northeastern Pacific into
   western North America, with large-scale ridging building across the
   Pacific Northwest, British Columbia and the Yukon Territory,
   downstream of digging large-scale troughing.  East of this feature,
   mid/upper flow is forecast to trend increasingly cyclonic across the
   Canadian prairies through the central Canadian/U.S. border area, as
   the center of a significant cyclone begins to shift/reform south of
   Hudson Bay.  As this occurs, a vigorous downstream short wave trough
   is expected to pivot northeastward, from the lower Great Lakes/upper
   Ohio Valley through much of the Northeast.  Models suggest that the
   increasingly sheared mid-level remnants of Harvey will become
   absorbed within the cyclonic flow to the east of this latter trough
   axis, and associated forcing for ascent may contribute to
   significant cyclogenesis, which is forecast to take place from
   northern Mid Atlantic coastal areas into the Canadian Maritimes
   Sunday through Sunday night.

   In the wake of the remnants of Harvey, a plume of seasonably high
   moisture content air is in the process of slowly advecting east of
   the Atlantic Seaboard.  A more rapid progression away from the coast
   appears likely on Sunday, while the plume also generally remains
   suppressed to the south, across the Florida peninsula and
   southeastern Gulf of Mexico.

   Given seasonably weak to modest moisture availability east of the
   Rockies, generally weak destabilization, at least where forcing for
   ascent may become supportive of convective development, seems likely
   to minimize the risk for severe storms.

   ...Northeast... 
   In the wake of considerable early period cloud cover and
   precipitation, insolation beneath the mid-level cold pool associated
   with the short wave impulse pivoting across the region may
   contribute to widely scattered thunderstorms from the lee of the
   lower Great Lakes into north Atlantic coastal areas Sunday.  Models
   suggest that the warm sector of the deepening surface cyclone could
   overspread southeast New England coastal areas late Sunday
   afternoon.  Given potentially strong vertical shear within this
   regime, severe weather potential may be non-zero given at least weak
   boundary layer destabilization, but due to the highly conditional
   nature of this risk, severe probabilities still appear below 5
   percent.

   ...Northeastern Minnesota...
   A regime characterized by strengthening deep layer wind fields/shear
   and lower/mid tropospheric warm advection, ahead of a significant
   southward advancing cold front, near or shortly after peak heating,
   could potentially become supportive of vigorous thunderstorm
   development Sunday afternoon and evening across the Minnesota
   Arrowhead vicinity.  However, at this time, it remains unclear that
   destabilization will become supportive of much beyond isolated storm
   development, and probabilities for severe hail and wind still appear
   to remain below 5 percent.

   ..Kerr.. 09/02/2017

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