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Storm Reports
Are you interested in what happened during a recent event? Check out the report below.
Severe Weather (March 1, 2007)
 
The satellite showed thunderstorms building into Arkansas from the north as a storm system ("L") dragged a cold front into the state from the Plains early on 03/01/2007. Severe storms developed from eastern Kansas into Missouri initially, and stayed there for several hours during the wee hours of the 1st. However, toward 4 am CST...the storms built toward the south into Arkansas.
In the picture: The satellite showed thunderstorms building into Arkansas from the north as a storm system ("L") dragged a cold front into the state from the Plains early on 03/01/2007.

 

Winds aloft changed direction with height, with rotation in some of the storms. As a result, Tornado Warnings were issued in northern sections of the state (in areas close to the Missouri border). The WSR-88D (Doppler Weather Radar) showed strong rotation in Fulton County (northern Arkansas) around 637 am CST on 03/01/2007.
In the picture: The WSR-88D (Doppler Weather Radar) showed strong rotation in Fulton County (northern Arkansas) around 637 am CST on 03/01/2007.

 

The sky was turbulent over northern Arkansas during the morning of 03/01/2007 Fortunately, there were no reports of damage. However, large hail was noted. Tennis ball size hail occurred at Norfork (Baxter County), with golfball size hail at Mount Judea (Newton County) and 8 miles southeast of Marshall (Searcy County).
In the picture: The sky was turbulent over northern Arkansas during the morning of 03/01/2007, with mammatus (pouch-like) clouds viewed near Franklin (Izard County). The photo is courtesy of Heidi Farrar. Click to enlarge.

 

Overall, the event was tamed a bit by marginal instability. In Arkansas, big severe weather outbreaks usually occur in the afternoon and evening...when daytime heating is at a maximum. In this case, while temperatures were above normal...warmer readings and a little more moisture could have made it much worse. Helicity and CAPE values were less impressive as sunrise approached on 03/01/2007.
In the picture: CAPE (Convective Available Potential Energy...or a measure of instability) values were held in check (below 1000 J/kg) during the early morning of 03/01/2007. At the same time, high helicity (representing the potential for rotating winds) values exited to the north and east of Arkansas. The graphic was constructed using data from the Storm Prediction Center in Norman, OK.

 

Plus, shear decreased rapidly toward sunrise...and was displaced into areas north and east of the state. Given this, the potential for rotating storms dropped.

Where instability and shear overlapped later in the day, numerous tornadoes were spawned from Alabama into Georgia. Nine people were killed around Enterprise in southeast Alabama, with eight deaths at a local school. Six more fatalities occurred near Newton in southwest Georgia.      

 

Temperatures at 7 am CST on 03/01/2007. In Arkansas, the event closed with cooler readings arriving behind a cold front. Temperatures dropped from the 60s into the 40s and 50s. It was also windy, with west to northwest winds at 15 to 25 mph and gusts over 30 mph.
In the picture: Temperatures at 7 am CST on 03/01/2007.

 

Storm Reports
Large hail occurred across northern Arkansas during the morning of March 1, 2007. For a look at some severe weather reports, click here.
Preliminary reports of severe weather in the Little Rock County Warning Area on March 1, 2007 (in red).
Submit a storm report.
In the picture: Preliminary reports of severe weather in the Little Rock County Warning Area on March 1, 2007 (in red).
 

 

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Page last modified: 15 November, 2007
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