Tornadoes · United States · Oklahoma · 1998

F0 tornado, Quinton, Oklahoma, May 6, 1998

This F0 tornado ran 0.3 miles across Pittsburg County on May 6, 1998, touching down at 8:32 PM CDT and reaching 30 yards wide. It killed nobody, and did $2,000 of property damage.

The rating scale

Tracks are drawn in the color of the rating. The Fujita scale rates the damage rather than measuring the wind: the speeds are what that damage is taken to imply.

  1. F040 to 72 mphthis tornado

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

  2. F173 to 112 mph

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

  3. F2113 to 157 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. F3158 to 206 mph

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

  5. F4207 to 260 mph

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

  6. F5261 to 318 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.

The record

Rating
F0
Date
May 6, 1998
Touchdown
8:32 PM CDT (01:32 UTC)
Path length
0.3 miles (0.5 km)
Path width
30 yards (27 m)
Deaths
0
Injuries
0
Property damage
$2,000
County
Pittsburg County
Touchdown point
35.120, -95.370
Lift-off point
35.120, -95.370
Record number
1021

What the Weather Service recorded

Summary of events for May 6:Numerous severe thunderstorms developed over eastern Oklahoma during the late afternoon and evening hours of May 6. Many of these thunderstorms developed rotation with some storms ultimately producing tornadoes. The first thunderstorms of the day developed over central Oklahoma and then moved eastward toward Okfuskee County after 430 PM CDT, traversing the counties along and just north of I-40 through 730 PM CDT before exiting into Arkansas to the east of Stilwell and Sallisaw. These thunderstorms produced large hail, numerous reports of funnel clouds, and two brief tornado touchdowns in Muskogee County. Other severe thunderstorms developed behind the first cluster, producing severe weather primarily in Creek and Okmulgee Counties from 700 PM to 830 PM CDT.Other severe thunderstorms developed rapidly around 600 PM CDT along a weak cold front across the northern border counties of Oklahoma. These storms primarily produced large hail. Further south in southeast Oklahoma, a cap of warm air in the mid-levels of the atmosphere prevented thunderstorm development until around 700 PM CDT with the approach of an upper level disturbance. Once thunderstorms developed in Pittsburg County, they rapidly became severe and began rotating. These storms moved east across Haskell and northern Le Flore Counties through 900 PM CDT, producing large hail, numerous reports of funnel clouds, several brief tornado touchdownsand a tornado producing considerable damage in the small town of Calhoun in northwestern Le Flore County. At the time of the Calhoun tornado, the WSR-88D near Fort Smith had its first algorithm-induced tornado vortex signature (TVS).

Emergency management director reported a tornado 4 miles southwest of Quinton. No known damage or injuries.

A brief tornado touchdown in Quinton knocked power lines down. There are no known injuries with this tornado. The parent storm produced a tornado 4 miles southwest of Quinton just five minutes earlier.

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

The warnings

2 minutes of warning. NWS TSA issued a tornado warning for this county at 01:30 UTC, 2 minutes before the tornado touched down, in force until 02:15 UTC.

Issued (UTC)ExpiredProductOffice
01:30 UTC02:15 UTCTornado WarningTSA

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 forecast that day

The Storm Prediction Center had this point in a Slight Risk. The outlook in force was issued at 11:01 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 air that afternoon

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.

Norman, OK (KOUN), 00:00Z

1.5 hours before the tornado, 185 km from the path. May 7, 1998.

Skew-T log-pSkew-T log-p diagram, Norman, OK at 00:00Z on 1998-05-07Temperature and dew point through the depth of the atmosphere, with the mixed-layer parcel lifted from the surface. Mixed-layer CAPE 1000 joules per kilogram, CIN -11, lifted condensation level 1337 meters above ground. Wind barbs in knots down the right edge.LCLLFCEL10008507005003002001001 km2 km3 km6 km9 km12 km15 km-30°-20°-10°10°20°30°40°
Temperature in red, dew point in green, the mixed-layer parcel dashed. The warm shading is its CAPE, the cool shading the inhibition it has to break through.
HodographHodograph, Norman, OK at 00:00Z on 1998-05-07The wind through the lowest 10 kilometers as a curve, rings every 10 meters per second labeled in knots. Zero to 1 km storm-relative helicity 81 square meters per square second, 0 to 6 km bulk shear 64 knots.1939587897117136156Sfc1 km3 km6 km9 kmRMLM
The wind turning with height, colored by layer: ground to 1 km, 1 to 3 km, 3 to 6 km, 6 to 10 km. RM and LM are the right and left moving storms Bunkers' method gives; the shaded area is the 0 to 1 km storm-relative helicity.
Mixed-layer CAPE
1000 J/kg
Mixed-layer CIN
-11 J/kg
Surface CAPE
2536 J/kg
Mixed-layer LCL
1337 m above ground
0-6 km bulk shear
64 kt
0-1 km bulk shear
14 kt
0-1 km storm-relative helicity
81 m²/s²
0-3 km storm-relative helicity
179 m²/s²
Significant tornado parameter
0.5
Supercell composite
5.4
0-3 km lapse rate
7.3 K/km

Open this sounding in Storm Lab

Norman, OK (KOUN), 12:00Z

10.5 hours after it, 185 km from the path. May 7, 1998.

Skew-T log-pSkew-T log-p diagram, Norman, OK at 12:00Z on 1998-05-07Temperature and dew point through the depth of the atmosphere, with the mixed-layer parcel lifted from the surface. Mixed-layer CAPE 0 joules per kilogram, CIN -43999, lifted condensation level 1538 meters above ground. Wind barbs in knots down the right edge.LCL10008507005003002001001 km2 km3 km6 km9 km12 km15 km-30°-20°-10°10°20°30°40°
Temperature in red, dew point in green, the mixed-layer parcel dashed. The warm shading is its CAPE, the cool shading the inhibition it has to break through.
HodographHodograph, Norman, OK at 12:00Z on 1998-05-07The wind through the lowest 10 kilometers as a curve, rings every 10 meters per second labeled in knots. Zero to 1 km storm-relative helicity -57 square meters per square second, 0 to 6 km bulk shear 76 knots.1939587897117136156Sfc1 km3 km6 km9 kmRMLM
The wind turning with height, colored by layer: ground to 1 km, 1 to 3 km, 3 to 6 km, 6 to 10 km. RM and LM are the right and left moving storms Bunkers' method gives; the shaded area is the 0 to 1 km storm-relative helicity.
Mixed-layer CAPE
0 J/kg
Mixed-layer CIN
-43999 J/kg
Surface CAPE
0 J/kg
Mixed-layer LCL
1538 m above ground
0-6 km bulk shear
76 kt
0-1 km bulk shear
5 kt
0-1 km storm-relative helicity
-57 m²/s²
0-3 km storm-relative helicity
95 m²/s²
Significant tornado parameter
0.0
Supercell composite
0.0
0-3 km lapse rate
2.5 K/km

Open this sounding in Storm Lab

The radar

The Western Arkansas radar (KSRX), 94 km away, was scanning. The volume nearest the touchdown began at 01:31 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.

This ground now

The live radar over the trackEvery 1998 tornado in OklahomaEvery tornado in Oklahoma since 1950Warnings in force in Oklahoma nowThe forecast where you are

The other tornadoes of May 6, 1998

7 more were confirmed in the United States that day.

DateTimeRatingWherePath (mi)Width (yd)DeathsInjuriesDamage
May 66:13 PM CDTF0Muskogee, OK0.130
May 66:21 PM CDTF0Muskogee, OK0.130
May 67:39 PM CDTF0Crawford, AR0.550
May 68:27 PM CDTF0Pittsburg, OK0.130
May 68:38 PM CDTF1LeFlore, OK0.81502$100,000
May 68:40 PM CDTF0Haskell, OK0.130
May 611:31 PM CDTF1Garland, AR3.0300$500,000

What this means

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.

Sources

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