EF0 tornado, Crosbyton Muni Arpt, Texas, June 4, 2012

1. EF065 to 85 mphthis tornado

   Light damage. Surface peeled off some roofs, gutters and siding damaged, branches broken, shallow-rooted trees pushed over.

2. EF186 to 110 mph

   Moderate damage. Roofs badly stripped, mobile homes overturned or badly damaged, exterior doors lost, windows broken.

3. EF2111 to 135 mph

   Considerable damage. Roofs torn off well-built houses, frame homes shifted on their foundations, mobile homes destroyed, large trees snapped or uprooted, cars lifted off the ground.

4. EF3136 to 165 mph

   Severe damage. Whole stories of well-built houses destroyed, large buildings badly damaged, trains overturned, trees debarked, heavy cars lifted and thrown.

5. EF4166 to 200 mph

   Devastating damage. Well-built houses leveled, structures with weak foundations moved some distance, cars thrown and large missiles generated.

6. EF5over 200 mph

   Incredible damage. Strong frame houses swept off their foundations, car-sized missiles thrown more than 100 meters, steel-reinforced concrete badly damaged, high-rise buildings deformed.

7. Unrated

   The survey recorded a tornado but could not put a number on it, most often because it crossed open country and damaged nothing a rating can be read from.

Rating

EF0

Date

June 4, 2012

Touchdown

8:28 PM CDT (01:28 UTC)

Path length

0.0 miles (0.0 km)

Path width

20 yards (18 m)

Deaths

0

Injuries

0

County

Crosby County

Touchdown point

33.630, -101.270

Lift-off point

33.630, -101.270

Record number

1206041928-01

Moisture trapped beneath a developing ridge of upper high pressure combined with strong daytime heating to fuel the development of numerous thunderstorms. Although wind shear was minimal, very strong instability led to several of these storms becoming strong while growing into multicellular clusters and lines. Some of these storms produced large hail, high winds and even one very brief EF0 tornado. The large coverage of these slow-moving storms proved very beneficial to South Plains residents and farmers as a widespread rain event had not occurred since early spring.

A brief tornado located about two miles southwest of Crosbyton was photographed by a storm chaser. NWS radar indicated a short-lived, low-level mesocyclone that developed along the northwest edge of an apparent surging gust front. The increased cyclonic shear to the left of the gust front's motion was likely stretched vertically and produced the brief EF0 tornado. No damage survey was conducted as the tornado was only in progress for less than one minute over open land.

From NOAA NCEI's Storm Events Database, the narrative the local forecast office wrote for Storm Data.

No tornado warning for this county appears in the archive as in force at the moment the tornado touched down.

Every warning and watch covering the touchdown point that day, from the Iowa Environmental Mesonet's archive of National Weather Service products. Lead time is measured from the issue of the warning in force to the touchdown time in the database, both of which were recorded to the minute by different people.

The Storm Prediction Center had this point in a Slight Risk. The outlook in force was issued at 00:59 UTC.

SPC's Day 1 convective outlook as it stood when the tornado began, read at the touchdown point. The same archive is on the radar archive.

The radiosonde launches on either side of the tornado, from the nearest station that was launching then, drawn and analyzed the way Storm Lab does: the same diagram, the same parcel and shear definitions SPC's mesoanalysis uses.

The Lubbock radar (KLBB), 50 km away, was scanning. The volume nearest the touchdown began at 01:30 UTC.

Open the radar archive at this moment, over the track

Reflectivity and velocity, decoded from the Level II archive in the browser. Volumes take a few seconds to open the first time.

Local storm reports within 60 km of the path, in the three hours either side.

From the Iowa Environmental Mesonet's archive of National Weather Service local storm reports.

The live radar over the trackEvery 2012 tornado in TexasEvery tornado in Texas since 1950Warnings in force in Texas nowThe forecast where you are

2 more were confirmed in the United States that day.

Ratings are the survey's, read off the damage rather than measured; the rating scale is above. Tornado counts rise through the record as reporting improved, so a year in the 1950s is not comparable with one today except for the strongest tornadoes, which were always noticed.

NOAA Storm Prediction Center tornado database, 1950-2025, the official record kept by NOAA's Storm Prediction Center.