Tornadoes · United States · Oklahoma · 1998

F0 tornado, Lamar, Oklahoma, March 30, 1998

This F0 tornado ran 0.6 miles across Hughes County on March 30, 1998, touching down at 5:18 PM CST and reaching 30 yards wide. It killed nobody.

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
March 30, 1998
Touchdown
5:18 PM CST (23:18 UTC)
Path length
0.6 miles (1.0 km)
Path width
30 yards (27 m)
Deaths
0
Injuries
0
County
Hughes County
Touchdown point
35.100, -96.130
Lift-off point
35.100, -96.130
Record number
333

What the Weather Service recorded

Summary of events of March 30th:A line of thunderstorms formed along a cold front as it moved east across central and southern Oklahoma. The line extended across the state from Kansas to Texas and produced large hail, damaging winds, and one tornado. The largest hail (golf ball-sized) was reported in Hickory in Murray County. Widespread wind damage occurred in Chickasha in Grady County as one storm evolved into a bow-echo. As the line of storms continued to move east, they developed comma-head radar signatures. One of these storms produced a small tornado (F0) in Lamar in Hughes County. See preceding individual Storm Data entries for further information and additional reports.

A severe thunderstorm produced a brief tornado in Lamar. Witnesses described a brief funnel that developed as the storm came across Lamar Mountain just southwest of town. This first funnel lifted and then a second funnel formed and touched down. The tornado moved north along the west edge of town for about .4 miles then veered to the northeast before lifting. On the southern end of the path, the roof was blown off a cow shed. Just north of there a travel trailer and dog house were blown over, an antenna was blown down, and a tree was uprooted. Shutters were blown off the next house to the north. About a block north of there the tornado blew the roof off a workshop and tossed a trampoline over a house. At this point the tornado turned to the northeast and destroyed a shed across from the post office and damaged a front porch. The damage path was about .6 miles long, and the tornado was rated F0.

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

The warnings

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

Issued (UTC)ExpiredProductOffice
22:46 UTC23:45 UTCSevere Thunderstorm WarningOUN

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 10:52 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), 12:00Z

11.3 hours before the tornado, 116 km from the path. March 30, 1998.

Skew-T log-pSkew-T log-p diagram, Norman, OK at 12:00Z on 1998-03-30Temperature and dew point through the depth of the atmosphere, with the mixed-layer parcel lifted from the surface. Mixed-layer CAPE 769 joules per kilogram, CIN -178, lifted condensation level 646 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 12:00Z on 1998-03-30The 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 231 square meters per square second, 0 to 6 km bulk shear 43 knots.1939587897117136Sfc1 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
769 J/kg
Mixed-layer CIN
-178 J/kg
Surface CAPE
621 J/kg
Mixed-layer LCL
646 m above ground
0-6 km bulk shear
43 kt
0-1 km bulk shear
39 kt
0-1 km storm-relative helicity
231 m²/s²
0-3 km storm-relative helicity
255 m²/s²
Significant tornado parameter
0.1
Supercell composite
0.9
0-3 km lapse rate
4.6 K/km

Open this sounding in Storm Lab

Norman, OK (KOUN), 00:00Z

0.7 hours after it, 116 km from the path. March 31, 1998.

Skew-T log-pSkew-T log-p diagram, Norman, OK at 00:00Z on 1998-03-31Temperature 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 -3000, lifted condensation level 672 meters above ground. Wind barbs in knots down the right edge.LCL10008507005003002001001 km2 km3 km6 km9 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 1998-03-31The 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 -325 square meters per square second, 0 to 6 km bulk shear 92 knots.1939587897117136Sfc1 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
-3000 J/kg
Surface CAPE
7 J/kg
Mixed-layer LCL
672 m above ground
0-6 km bulk shear
92 kt
0-1 km bulk shear
22 kt
0-1 km storm-relative helicity
-325 m²/s²
0-3 km storm-relative helicity
-26 m²/s²
Significant tornado parameter
0.0
Supercell composite
0.0
0-3 km lapse rate
4.4 K/km

Open this sounding in Storm Lab

The radar

The Norman radar (KTLX), 107 km away, was scanning. The volume nearest the touchdown began at 23:18 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 March 30, 1998

2 more were confirmed in the United States that day.

DateTimeRatingWherePath (mi)Width (yd)DeathsInjuriesDamage
March 305:35 PM CSTF1Wapello, IA0.230$10,000
March 308:25 PM CSTF1Benton, AR1.2130$100,000

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.