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Overview

Several severe storms developed along and ahead of a cold front/dryline as it moved towards the Ozarks on the evening of March 23, 2016. Moisture from the Gulf of Mexico was able to stream north into the region with the aid of a strong 850mb low level jet. Strong shear in association with synoptic winds and strong 850mb winds combine with limited instability were enough to produce a tornacic storm that moved across Barry into Stone Counties in Missouri. The very strong shear was able to overcome the limited instability as a strong storm embedded in a line of storms, moved across southern Missouri. This storm ultimatly developed an EF-1 Tornado near Shell Knob, Missouri.

Image

Damage from near Shell Knob
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Shell Knob Tornado - Reflectivity Shell Knob Tornado - Storm Relative Velocity Shell Knob Tornado - Correlation Coefficient

Tornadoes:

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Tornado - Near Shell Knob, MO
Barry and Stone Counties

Date March 23rd, 2016
Time (Local) 12:08 AM CDT
EF Rating EF-1
Est. Peak Winds 97 MPH
Path Length 3.80 Miles
Max Width 200 Yards
Injuries/Deaths 0

Summary:

EF-1 tornado touched down 1 mile northeast of Shell Knob and tracked nearly 4 miles northeast and terminated just after crossing Piney Creek Cove of Table Rock Lake.  Damage was mainly limited to uprooted and snapped trees.

Track Map

Track Map EF-Scale

 

Radar/Photo  
Tornado damage near Shell Knob Tornado Damage near Shell Knob Tornado Damage near Shell Knob  

 

The Enhanced Fujita (EF) Scale classifies tornadoes into the following categories:

EF0
Weak

65-85 mph
EF1
Moderate
86-110 mph
EF2
Significant
111-135 mph
EF3
Severe
136-165 mph
EF4
Extreme
166-200 mph
EF5
Catastrophic
200+ mph
ef-scale

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Storm Reports

 


 

 


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