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EF2 tornado in Ochiltree County, Texas

Tornado May 23, 2019 · Ochiltree County, Texas

EF2
Rating
17.5 mi
Whole path
900 yd
Path width

NOAA records this tornado county by county. Its path ran through Roberts County → Ochiltree County → Lipscomb County; the totals above are for the whole tornado.

EF0EF1EF2EF3EF4EF5Unrated

The path drawn at its surveyed width of 900 yards (0.51 mi) — zoom in and the swath grows to true scale. Other tornadoes recorded nearby that day are shown faint.

What EF2 means. On the Enhanced Fujita scale, EF2 is considerable damage: roofs torn off well-built houses, mobile homes destroyed, large trees snapped or uprooted, consistent with estimated gusts of 111–135 mph. The rating comes from a survey of the worst damage after the storm, not from a wind measurement, so it says as much about what the tornado hit as about how strong it was.

What the National Weather Service wrote

The tornado touched down in northern Roberts County around 659 pm CDT, crossed the Roberts/Ochiltree county line around 704 pm CDT and the Ochiltree/Lipscomb county line around 719 pm CDT before dissipating through a rope out process by 733 pm CDT. Damage from the tornado consisted mostly of damage to trees, power lines and

oil/natural gas field equipment and sheds. There was also two manufactured homes being transported via truck the were blown off Highway 83. The tornado was noted to be larger and possibly stronger in inaccessible open county to the southwest of

the location where it was measured to be around 1/2 mile wide and rated an EF2 by the survey team.

The wider storm

A vigorous upper level low pressure system developed across southern Nevada. Significant wind shear and instability developed as moisture was drawn north into the Panhandles setting the stage for a very long duration and higher end severe episode. Initially, elevated supercell storms developed in the NW Texas Panhandles on the cold side of a nearly stationary frontal boundary and moved northeast into the central Oklahoma Panhandle as the first of multiple disturbances moved across the area. Hail up to golf ball size and wind damage was reported with these storms.

During the afternoon hours, upper level disturbances, daytime heating and the very pronounced frontal boundary stretching from near Amarillo northeast into Beaver County, Oklahoma became the main catalyst for surface based supercells, which produced very large hail up to baseball size and several tornadoes. Two very large and long tracked tornadoes produced damage across the northeast Panhandles. Both were rated EF-2s based on the damage, but they remained in very rural areas throughout their life-cycle. A total of eight tornadoes occurred during this event, however three of these were landspouts that developed along an outflow produced by storms early in the event. With the loss of daytime heating, supercells congealed into a line which produced gusty winds and hail across the eastern Texas Panhandle before finally moving east and exiting the region in the early morning hours on May 24th.

Began near Farnsworth (36.0567, -100.6423).

Other tornadoes from the same storm system

7 more tornadoes the National Weather Service filed under this storm episode.

Source: NOAA Storm Events Database, event 830292. Narratives are written by the National Weather Service forecast office that issued the report.

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