Aug 17, 2020 1730 UTC Day 2 Convective Outlook
Updated: Mon Aug 17 16:56:18 UTC 2020 (20200817 1730Z Day 2 shapefile | 20200817 1730Z Day 2 KML)
Probabilistic to Categorical Outlook Conversion Table
Categorical Graphic
20200817 1730 UTC Day 2 Outlook Graphic
Day 2 Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
MARGINAL 148,880 1,033,290 Missoula, MT...Bozeman, MT...Lewiston, ID...Butte, MT...Helena, MT...
Probabilistic Tornado Graphic
20200817 1730 UTC Day 2 Tornado Probabilities Graphic
Probability of a tornado within 25 miles of a point.
Hatched Area: 10% or greater probability of EF2 - EF5 tornadoes within 25 miles of a point.
Day 2 Tornado Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
No Risk Areas Forecast
Probabilistic Damaging Wind Graphic
20200817 1730 UTC Day 2 Damaging Wind Probabilities Graphic
Probability of damaging thunderstorm winds or wind gusts of 50 knots or higher within 25 miles of a point.
Hatched Area: 10% of greater probability of wind gusts 65 knots or greater within 25 miles of a point.
Day 2 Wind Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
5 % 148,873 1,014,493 Missoula, MT...Bozeman, MT...Lewiston, ID...Butte, MT...Helena, MT...
Probabilistic Large Hail Graphic
20200817 1730 UTC Day 2 Large Hail Probabilities Graphic
Probability of hail 1" or larger within 25 miles of a point.
Hatched Area: 10% or greater probability of hail 2" or larger within 25 miles of a point.
Day 2 Hail Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
5 % 54,724 306,327 Garden City, KS...Dodge City, KS...North Platte, NE...Liberal, KS...Lamar, CO...
   SPC AC 171656

   Day 2 Convective Outlook  
   NWS Storm Prediction Center Norman OK
   1156 AM CDT Mon Aug 17 2020

   Valid 181200Z - 191200Z

   ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS ACROSS PORTIONS
   OF THE NORTHWEST...AND OVER PARTS OF THE WEST-CENTRAL PLAINS...

   ...SUMMARY...
   Isolated severe thunderstorms -- accompanied by risk for damaging
   winds -- are forecast to spread across parts of the Northwest on
   Tuesday, from eastern Oregon into parts of western Montana.  A
   couple of severe storms may also occur over the west-central Plains
   vicinity.

   ...Eastern Oregon into western Montana...

   Strong west to southwesterly flow will spread across the Northwest
   atop the amplified upper ridge on Tuesday. Weak shortwave
   perturbations will migrate through the flow, and aid in diurnally
   induced thunderstorms. Forecast soundings indicate modest
   instability with MLCAPE values as high as 500-1000 J/kg amid 30-50
   kt effective shear. Low level flow will be rather weak beneath high
   cloud bases, but fast mid/upper flow will result in quick storm
   motions. Very steep low level lapse rates with inverted-v low level
   thermodynamic profiles are expected, which will aid in strong
   downdrafts. As a result, locally severe storms capable of strong
   gusts are possible from late afternoon into the evening hours.

   ...West-Central Plains...

   A somewhat conditional severe threat will exist across parts of
   southwest NE, far eastern CO, western KS and possible as far south
   as the OK Panhandle late Tuesday afternoon into the evening. The
   Great Plains will be under moderate north/northwest mid/upper level
   flow to the east of the western upper ridge. Most guidance shows
   weak perturbations migrating through northwesterly flow. However,
   strong capping will preclude thunderstorm development for much of
   the day. By late afternoon or evening, a few storms could develop as
   the boundary layer mixes and inhibit weaken sufficiently amid
   moderate instability (MLCAPE 1500-2500 J/kg). The surface pattern
   will remain rather nondescript, with the only feature noted being a
   surface trough/dryline extending north-to-south through the High
   Plains. Surface dewpoints will generally be from the upper 50s to
   mid 60s east of the boundary with strong heating resulting in deep
   mixing through peak heating. High-based cells will mainly be capable
   of strong downburst winds in this steep low level lapse rate
   environment. Winds will be rather weak in the low levels, but
   south/southeasterly winds beneath north/northwest upper flow will
   result in 35-45 kt effective shear. With sufficient instability in
   place, the strongest cells, should they form, could also produce
   hail.

   ..Leitman.. 08/17/2020

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