Summary of the March 2nd 2012 Tornadic Supercells
On Friday March 2nd, 2012, tornadic supercells that developed
in central and eastern Kentucky tracked into West Virginia. These
storms were responsible for two deaths, an undetermined amount of
injuries, and large areas of destruction within the Charleston, WV
(RLX) National Weather Service WFO county warning area.
On the morning of March 2nd, a deep upper- level trough over
the central plains began lifting northeastward into the Ohio River
Valley, with maximum jet speeds of 125mph. At the surface, low pressure
centered near Missouri began to deepen and move northeastward toward
the southern Great Lakes region. By early afternoon, a warm front was
positioned from southern Illinois, across Kentucky, southeastward into
the Tennessee River Valley. In response to strong southerly flow,
dewpoints across much of Kentucky began to exceed 60F. Late in the
afternoon, the cold front began moving across central Kentucky as the
surface low began to occlude, and the warm front stalled over central
West Virginia.
At 6pm, a number of supercells ahead of the cold front were
moving across southeast Ohio, central Kentucky and eastern Kentucky.
The strongest moved through West Liberty, KY, causing 8 deaths. This
supercell entered the RLX county warning area (Lawrence County, KY) at
approximately 6:10pm before dissipating over Lincoln County an hour
later at approximately 7:10pm. It was responsible for 2 deaths in
Lawrence County, Kentucky along with extensive damage in Dunlow and
Kiahsville, West Virginia.
 |
|
FIG. 1. SPC MCD #0215 At
215pm the Storm Prediction Center issued a Mesoscale Discussion
outlining an area that was favorable for strong destructive tornadoes
in the late afternoon.
|
 |
| FIG. 2 Tornado Watch #62 At 420pm the SPC issued a Tornado Watch covering Eastern Kentucky, western West Virginia, and southeast Ohio. |
Storm 1 - Lawrence KY and Wayne County WV
 |
| FIG. 3 This tornado path was almost 53mi long, and reached EF-3 strength. |
|
 |
| FIG. 4 Basic Reflectivity of a classic hook echo as it crossed Wayne County. |
|
 |
| FIG. 5 This is the Base Velocity at the same time and position. This helps us determine the magnitude of the circulation. |
|
Storm 2 - Lincoln County WV
 |
| FIG. 6
This path was almost 16mi long. Rated an EF-1, it originated very
close to where the long track tornado dissipated 30min earlier. |
|
 |
| FIG. 7 Basic Reflectivity as the storm moved over Lincoln county |
|
 |
| FIG. 8 Base Velocity at the same time and position showing the tight circulation. |
|
 |
| FIG. 9 Storm2 moving in behind Storm1 |
|
Storm3 - Mingo County WV (Magoffin County KY, Johnson County KY, Martin County KY)
 |
| FIG. 10 The storm wasn't in Mingo County long, but it did extensive damage to a 60 ft. communication tower. |
 |
| FIG. 11 The entire track as it moved east toward Mingo County |
 |
| FIG. 12 Base Reflectivity entering Mingo County |
 |
| FIG. 13 B ase Reflectivity west of Mingo County with a distinct hook echo at 0024z |
 |
| FIG 14. Base Velocity entering Mingo County |
 |
| FIG. 15 Base Velocity west of Mingo county at 0024z |
We will be updating this summary as we gather more
information. Please contact us with any information you may have on the
storms, especially pics! Also, don't hesitate to ask us questions
either by email or facebook.