Saturday, May 23, 1998

Location: Owensboro, KY
What Was Seen: Non-Tornadic Supercell Thunderstorm
Time: 10:48 PM CDT

[CLICK ON IMAGE TO ENLARGE]

Summary...

Well, to start off, the entire time period from May 19 to May 24 was quite something. With a nearly stationary front poised across the Ohio Valley, separating very warm and moist air to the south from much cooler and drier air to the north, storm complexes rolled through daily (sometimes...several times a day). May 23rd saw much of the same...except a southern stream shortwave enhanced the low- and mid-level flow across the area, creating a better vertical wind-shear profile than in previous days.

Early that evening (the 23rd), storms began to fire in S. Illinois and S.W. Indiana (as expected)...with a strong tail-end cell blowing-up right under the left-exit quadrant of the sub-tropical jet max, located near the apex of the Kentucky/Indiana/Illinois borders (in Posey Co. Indiana), around 9:30 PM CDT. The cell quickly became severe and started taking a more easterly track...as compared to the north-easterly track most of the other storms in the area exhibited. As this particular storm moved south of Evansville, IN, doppler radar showed VILs in the 55-65 kg/m^2 range and moderate storm-relative rotation. Following the Ohio River eastward, the storm moved into Owensboro around 10:45 PM CDT. Doppler radar at Fort Knox, KY (LVX) detected a weak mesocyclone with the storm at this time. A distinct rear-flank-downdraft (RFD) and associated inflow notch became visible in the radar reflectivity pattern as the storm approached Owensboro from the west (see KLVX radar image BREF1). The storm continued to skirt along the Ohio River which placed the RFD/pendant echo (hook-type echo) directly over the city between 10:40 and 10:50 PM CDT.

At this time, it does not appear that any tornadic activity was associated with this storm. After viewing the damage pattern the next day, I concluded that the wind damage that occurred in the central and northern sections of the city appeared to be caused by straight-line, RFD-type winds. Regardless, there was extensive tree and power line damage across these areas of the city. Several large trees were completely uprooted or broken off at the base with many very large limbs downed as well...many downed across roads. Fallen trees also knocked down quite a number of power lines and a few utility poles. Some minor structural damage also occurred...again, mainly due to fallen trees. Needless to say, power (which had also been knocked out by storms the previous night) was out again in many of the same areas in the central sections of Owensboro.

The storm held its own and continued on an eastward trek... It even strengthened some later that night as it moved toward central Kentucky. Becoming a rather long-lived storm cell, it eventually wreaked havoc in areas farther east across central and eastern portions of the state (even past 3 AM) with several reports of large hail.

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Last Updated: May 24, 1998
Dave Demko