Convective Outlook

U.S. Severe Weather Forecast

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acus02 kwns 191732 
swody2 
Storm Prediction Center ac 191730 


Day 2 convective outlook 
National Weather Service Storm Prediction Center Norman OK 
1230 PM CDT Wednesday Jun 19 2013 


Valid 201200z - 211200z 


..there is a slight risk of severe thunderstorms Thursday and Thursday night 
across parts of the northern plains into upper Mississippi Valley... 


... 
The eastward progression of a broad closed low...now near the 
Pacific northwest coast...appears likely to remain slow through this 
forecast period. Variability exists among the model data... but 
mostly in response to a significant impulse pivoting around its 
eastern and northern periphery...the circulation center is expected 
to only reach somewhere between the Columbia Plateau and the 
northern rockies by late Thursday night. 


Downstream...large-scale upper ridging is expected to persist across 
eastern portions of the northern plains into the upper Mississippi 
Valley. But this feature may be modulated by smaller scale 
perturbations emanating from cyclonic flow to the south of the 
closed low...across the Great Basin and north central rockies 
through the crest of the ridge across the upper Midwest. 


Farther east...weak middle/upper troughing probably will linger across 
much of the southeast...to the south of relatively strong ... 
generally confluent middle/upper flow regime across eastern Canada and 
adjacent areas of the upper Great Lakes into New England. 


..northern plains into upper Mississippi Valley... 
Downstream of the northwestern U.S. Closed low...very warm and 
deeply mixed boundary layer air emerging from the intermountain west 
and rockies region is forecast to advect east of the higher 
terrain...through much of the Great Plains by late Thursday 
afternoon. This will occur above lower level moistening on modest 
southerly flow ahead of a surface trough developing to the Lee of 
the northern and central rockies...and contribute to significant 
destabilization. Steep middle-level lapse rates...coupled with 
boundary layer moisture characterized by middle/upper 60s surface dew 
points...are expected to contribute to a sizable area of moderate to 
large cape /in excess of 2000 j per kg/. 


Thermodynamic profiles across the region will certainly be 
supportive of severe storm potential...including the risk for very 
large hail...at least localized strong and damaging convective wind 
gusts...perhaps a few tornadoes. The environment probably will be 
conducive to the development supercells and the upscale growth of 
one or more sustained...organized storm clusters. 
However...considerable uncertainty remains concerning the location 
and details of convective development and evolution Thursday and 
Thursday night. This is largely due to model variability concerning 
the smaller scale features...and their impact on the flow fields and 
shear across the region...which may be characterized by weaknesses 
at various levels compared to days with more clear-cut severe 
weather potential. 


It currently seems possible that forcing associated with a weak 
impulse progressing into/through broader scale anticyclonic 
flow...around the northern periphery of the more strongly capping 
elevated mixed layer air...will contribute to the initiation of 
discrete storms by late Thursday afternoon across parts of the 
central and eastern Dakotas. A subsequent increase in storm 
development...gradual consolidation and upscale growth into a large 
mesoscale convective system then appears possible eastward toward 
the upper Mississippi Valley during the evening hours. This may be 
aided by a nocturnally strengthening southerly 850 mb 
jet...northeast of the middle Missouri Valley through portions of 
Minnesota/Wisconsin. 


..southern High Plains into parts of the Central Plains... 
Forcing for convective development near the Lee surface trough 
remains unclear. However...strong surface heating and deep boundary 
layer mixing may overcome inhibition and allow for the initiation of 
scattered storms off the higher terrain and south/ east of the 
southeast Colorado thermal low. If this occurs...thermodynamic 
profiles will be conducive to strong convective surface 
gusts...perhaps some hail. Strong wind gust potential could persist 
with lingering convection after dark... aided by low-level jet 
intensification across the Texas/Oklahoma Panhandle region into 
western Kansas. 


.Kerr.. 06/19/2013